Geco9)G58X- L8i -/03National Uranium Resource EvaluationAERIAL GAMMA RAYWAYCROSSGEORGIAAND MAGNETIC SURVEYAND BRUNSWICK QUADRANGLESFINAL REPORTtie~ %x0FY< EGG GEOMETRICSSunnyvale, California 94086March 1981umW~ATESOPREPARED FOR U.S. DEPARTMENT OF ENERGYGrand Junction Office, Coloradometadcl202330G BX -I,This report is a result of work performed by EG&G geoMetrics through aBendix Field Engineering Corporation Subcontract, as part of theNational Uranium Resource Evaluation. NURE is a program of the U.S.Department of Energy's Grand Junction, Colorado, Office to acquire andcompile geologic and other information with which to assess themagnitude and distribution of uranium resources and to determine areasfavorable for the occurrence of uranium in the United States.This report was prepared as an account of work sponsored by an agencyof the United States Government. Neither the United States Governmentnor any agency thereof, nor any of their employees, makes any warranty,express or implied, or assumes any legal liability or responsibilityfor the accuracy, completeness, or usefulness of any information,apparatus, product, or process disclosed, or represents that its usewould not infringe privately owned rights. Reference herein to anyspecific commercial product, process, or service by trade name, trade-mark, manufacturer, or otherwise, does not necessarily constitute orimply its endorsement, recommendation, or favoring by the United StatesGovernment or any agency thereof. The views and opinions of authorsexpressed herein do not necessarily state or reflect those of theUnited States Government or any agency thereof.1vrfl~77r777 r 7- ___...........i1U J T T LJY1 ir: L 1 L JAERIAL GAMMA RAY AND MAGNETIC SURVEYWAYCROSS AND BRUNSWICK QUADRANGLESGEORGIAFINAL REPORTPrepared byEG&G geoMetricsSunnyvale, CaliforniaMarch 1981Prepared for the U.S. Department of EnergyGrand Junction Office, ColoradoUnder Contract No. DE-AC13-76GJ01664and Bendix Field Engineering CorporationSubcontract No. 80-426-L-1-ABSTRACTThe Waycross and Brunswicksquare miles of land in soutately thick sections of theposures are entirely Tertiaryquadrangles cover approximately 11,000heast Georgia. The area overlies moder-Southeast Georgia Basin. Surficial ex-to Recent deposits.A search of available literature revealed no known significant uraniumdeposits.Adialtotal of fifty-eight (58) uranium anomalies were detected and arescussed briefly in this report. None were considered significant and1 appear to be related to cultural features.Magnetic data poorly reflects existing structural interpretation.Numerous linear and isolated high gradient features dominate the area,and appear to express complexities in the Paleozoic and older basementmaterial.-ii-ITABLE OF CONTENTS LIST OF FIGURESPage Nos.Page Nos.I. INTRODUCTIONGeneralPhysiography11Figure 1 Location MapFigure 2 Tectonic Structure MapII. GEOLOGYStructureSurface GeologyUraniumIII. INTERPRETATION OF GEOPHYSICAL DATARadiometric DataMagnetic DataIV. BIBLIOGRAPHY22233335Figure 3 -Uranium Anomaly/Interpretation MapFigure 3a Uranium Anomaly/Interpretation MapV. APPENDICESAppendix A -AppendixAppendixAppendixAppendixAppendixBCDEFAppendix G -Appendix H -Data Acquisition, Processing, andInterpretation MethodsFlight SummaryFlight Path and Geologic MapProfilesStandard Deviation MapsHistograms and Map Unit ConversionTableUranium Anomaly Summary andStatistical TablesPseudo-Contour Maps1244a-iii-INTRODUCTIONGeneralThe Waycross and Brunswick quadrangles contain approximately 11,000square miles of land area in southeastern Georgia (see Figure 1).The geologic maps used in the interpretation were compiled by MartelLaboratories, Inc., in 1980. Both maps were compiled at a scale of1:250,000 from a state geologic map of 1:500,000. Outlined units onthe two maps do not register exactly (up to .5 km) along the commonborder, as well as inaccuracy due to approximate geologic contacts.This casts some doubt on the accuracy of the digitized units used inthe interpretation. Geologic map unit descriptions, found in AppendixC, were taken directly from the Martel map legends. Supplementarygeologic information was taken from Murray (1961), Fairbridge (ed.)1975, Flint (1971), Florida Special Publication, No. 5, and Cohee andothers (1962). Cultural and physiographic data were taken from the1:250,000 scale Waycross (1966 version) and Brunswick (1968 version)topographic maps.Radiometric and magnetic data for both Waycross and Brunswick quad-rangles were acquired in January of 1981, and processed in March. Adetailed summary of data acquisition, processing, interpretation, andpresentation methods can be found in Appendix A of this report.Appendix B contains a flight summary report for the two quadrangles.It should be noted that although Appendixes C, D, E and H are presentedas separate quadrangles, the intepretation reports, statistics, datatapes and microfiche are processed and presented as one area.PhysiographyThe area defined by the two map sheets lies within the eastern plainsof the Atlantic Coastal Physiographic Province. The gently-seawarddipping topography is dominated by agriculture and poorly forested land("sand barren"). Barrier beaches with interior marshes and swamps areprominent along the coastal region. The region is largely drained byseveral rivers and bayous that flow southeastward directly into theAtlantic Ocean, with the exception of the western third of the regionwhich essentially drains southward. The largest river in the region isthe Altamaha River, which flows from the northcentral border (where theOcmulgee and Oconee Rivers merge and form the Altamaha River) to theAtlantic Ocean. The Ocmulgee River controls drainage in most of thenorthwestern border area until it merges with the Oconee River, whereit enters into the Altamaha River watershed to the east. West andsouth of the Ocmulgee and Altamaha Rivers is a series of smaller riversdraining the remaining 70 percent of the area. These include: Satilla,Alapaha, and Little River Rivers (from east to west respectively),noting that the inter-river regions are typified by slightly elevatedterraces and rugged uplands.The topography varies from flat to gently sloping in the coastalplains, to rough, irregular uplands in the west. Elevations rangefrom sea level, to over 500 feet in the northwestern quadrant. Much0WW0Aw-r .Mq r(9ain r n xorrriim ehs k R i mEr Murrs e}e s/Lenoir .iT E.N- N S 4 "E.. ,.WilcAshebO 0 ' ilas Comlna s byv ile AsHw +c ory6CA RN a -N vll A R l s borore sPurgT Gastonia lbermarle Sanf&"' .. ayetteville I CI aefn ,,1(AT PAR 4w8fS-eSpartan r F ettevdle~.thi uflts ite ~-' -as- .Rck H Lauriilbuirg Jackcson~vlllttC.or ' ..,Ml ; AeturToccoa ' Andersoni LU ofenn NLumberton AT'Gunt rvke ra Ga ne vle -twe L8i S -+"~ser addrt__L~N a, -- s~'G~wood .- ~~aFlyrence N;:-'"---t;*' Ianta Not CAROI N LakeCit Myte BeachBesseme , .,fTalladga East c' Covsrt N-Pug Aikeneb ,"tGeorgetown1 ! ra iatKp -o.FLOR IDA'F caa ,- TDaytona BeachDe Land,'/ *New Smyrna BeachLesburg . SafordO land TitusvilleCocoTa , .MelbourneClearwate c/ Winter HavenSt Petersburg BartowVeroBeachSeb\ Fort Pierce BAHAMA-Sarasota Okee hobee ISLANDS".Arcadia ,Punta Gorda'.> _ .Palri;_PunBeachPalm BeachFort Myers 1 Lake Worth -Naples pompano ea rtLauderdale\- .WoodLOCATIlON DIAGRAM-l NS NORTH CAROLNANI 15.9 N! 17 7 I AiJaiTA 1. NI 179I '. SOUTH.AON Y -CAROLI IAIg NI 17.10 I N1 17-1 ii I NI 17.12Q NI 1&t2 GEORGIA .A~ NNH'15.3 NH 17.1 NH 172*OOTi'AN NYC"iSg , B " NSiN 166- NAL NASt7 NH 17.45FLORIDA JACK SO44"I"; y.* CANESVhENH169 NH 17.7 NHa1A8429 i 293' 76FIGURE 1LOCATION MAPWAYCROSS AND BRUNSWICKQUADRANGLESScale100 5035 N300N-1-100 MILESII-I IIof the coastal plain lies below 50 feet, with the exception of a largebarrier island deposit located in the southern portion of the coast.The area is moderately developed culturally. The largest cities areWaycross and Brunswick, both with populations exceeding 17,000. FortStewart overlies the northern half of the coastal area. The entireregion is dotted with smaller cities and towns, and contains an exten-sive network of roads and railraods with numerous interstate highwaysextending across the quadrangle.GEOLOGYStructureThe region lies over the Southeast Georgia Embayment between thePeninsular Arch to the southwest and the Appalachian Foldbelt to thenorthwest (see Figure 2). The structural picture of the region duringLower Cretaceous to Recent times defers markedly from the underlyingolder sequence, as shown by test well data. These Cretaceous andyounger aged deposits appear to rest with angular unconformity, andonlap, on the Paleozoic and older basement material of the Appalachianand Ouachita foldbelts. The Cretaceous and younger age deposits rangein thickness from 1500 feet in the northwest corner to over 4500 feetalong the eastern coastline, with thicker sediments lying offshore.There are no known faults in surficial or Paleozoic deposits accordingto Martel Laboratories and Cohee and others (1962).Surface GeologyAs mapped by Martel Laboratories, Cenozoic sedimentary material coversthe entire surface of the region, with Tertiary exposures accountingfor 40 percent of the area and Quaternary exposures covering 30 percent.Part of the Quaternary system consists of alluvial, less, and eoliansand deposits, all of Holocene age. These deposits account for 5percent of the surface. Alluvium is mapped only within the floodplainsof the major river systems within the eastern two-thirds of the area.Pleistocene deposits consist of barrier island and marsh deposits andaccount for 15 percent of the surface. These Pleistocene sediments arealluvial deposits from interglacial periods ranging from early Sangamonto late Peorian stages. Pleistocene-Pliocene sands and gravels,undifferentiated, account for approximately 30 percent of the surfaceand was mapped within the low lying coastal plains in the easterntwo-thirds of the area.Tertiary deposits consists of Eocene to Miocene sands, clays, marls,and limestones. The Miocene Hawthorne Formation (southwest quadrantexclusively) contains minor to trace amounts of phosphate particles.This formation accounts for 15 percent of the total surface. Theremaining 25 percent was mapped as undifferentiated Pliocene andMiocene sedimentary rocks. These sedimentary rocks dominate thenorthwestern quadrant.80 WFR' - /- - t m2500--A o w/' I V-ALDC ST AWaycross.,-I Ii .~.~,SSELAKE C!T-1N r,N /2 KAfterUSGS and AAPGTectonic Map of the United StatesbyCohee and others (1962)I,25FIGURE 2TECTONIC STRUCTURE MAPWAYCROSS AND BRUNSWICKQUADRANGLESScale 1:2,500,0000 25 50 75 MILES0=25 50 75 MILES-7Brunswi/oYflQiAi i r/- j..---. //lJij '-Trr32 N310 N-2-5a000 --I-r-- i - ! -r ,I,iI84"W 02W *~ u/TMiII- - - .,.2E ITertiary age materials were deposited in a series of alternating marinesubmergence and emergence. Eocene Ocala limestone is a major aquiferin the region. The environment ranges from shallow marine platform tolow energy nearshore environments with intermittent emergence. TheHawthorne Formation was probably exposed during late Miocene time,forming karst topography and accumulations of phosphatic residuum,(Altschuler and others, 1960).UraniumAccording to available sources, there are no known significant uraniumdeposits, though phosphoritic sediments contain concentrations ofuranium that are known to be higher than the adjacent rock units(Altschuler and others, 1960 and Cathcart, 1955).INTERPRETATION OF GEOPHYSICAL DATARadiometric DataA total of 58 groups of uranium (Bi214) samples meet the minimumstatistical requirements set forth in the data interpretation sectionof Appendix A. These are displayed, along with all other anomaloussamples and pertinent data, on Figure 3 and 3a. The anomalies aresummarized in a table in Appendix G. The potassium, uranium, thorium,and ratio pseudo-contour maps, which reflect radiometric responses foreach quadrangle, are found in Appendix H. Discussion of the abundancesof potassium, uranium, and thorium are in terms of apparent equivalentpercent and apparent equivalent ppm. These equivalent units arederived from scaling of counts per second by the sensitivities calcu-lated for the detection system and as such cannot be taken as directlydetermined geochemical values.Concentrations of the three radioactive elements are extremely low.The overall average uranium concentration is 1.6 ppmeU. The averagepotassium and thorium concentrations are .2 percent and 4.0 ppmeTrespectively. Map unit QAL (Recent alluvium) contains both the peakand highest average uranium concentrations at 4.65 ppmeU and 1.93 ppmeUrespectively. Map units QTPAM (Quaternary Pamlico terrace marshdeposit) and TPMU (Pliocene and Miocene sedimentary rocks, undifferen-tiated) have only slightly less concentrations (avcragely-(2-ppmeU).Thorium concentrations reach a peak of 16.4 ppmeT in map unit QTPRAM(Quaternary Princess Anne terrace marsh deposits), and also map unitQTPAM contains the highest average thorium concentration at 6.0 ppmeT.Peak concentrations of potassium occurs in map unit QTPPS (Pleisto-cene - Pliocene sands and gravels, undifferentiated) at 1.54 percent,while map unit QAL contains the highest average concentration of 0.28percent.In general, highest concentrations of potassium, thorium, and uraniumare confined along the northern border and most of the Brunswickquadrangle (see Appendix H). The remainder of the area containssomewhat uniform concentrations of the three elements and valuesgenerally less than the area-wide average concentrations. The higherconcentrations along the northern border are mainly due to alluvium,with minor contributions by the adjacent map unit TPMU. The higherconcentrations within the alluvium appears to contain source materialfrom outside the area (probably Appallachians). In the Brunswickquadrangle all three elements moderately vary in concentrations overshort lateral distances. The large variations in concentrations arepartially due to marshes and other water bodies which cloud the dis-tinction of the different terrace deposits (on the pseudo-contour map).The higher concentrations are mainly due to alluvium, and a couple ofPleistocene terrace deposits. In general the Pamlico and Princess Anneterrace deposits contain higher concentrations of all three radioactiveelements and only slightly higher than the alluvium deposits.Anomalies are scattered throughout the area, but tend to cluster in thenorthern border of the Waycross quadrangle and the south-centralportion of the same quadrangle. Over half the anomalies are attributedto alluvium and map unit TPMU. Map units QTPPS is the next dominantunit, and is found mainly in the central portion of the Waycrossquadrangle. Peak concentrations in these anomalies range from 1.8 to4.6 ppmeU, with all anomalies above 3.8 ppmeU being attributed toalluvium. All of the anomalies appear to be associated with culturalfeatures of some sort (such as roads, railraods, cities, etc.).The low uranium concentrations, coupled with the correlation toculture, suggest that none of the anomalies depicted in this reportshould be considered as reflecting possible uranium concentrations.Magnetic DataThe magnetic field pseudo-contour maps appear in Appendix H.The region contains a thickening sequence of Mesozoic and Cenozoicdeposits from west to east. Though the structural configuration of theunderlying Paleozoic strata is not well known, it is thought to be ofsubstantial thickness.The magnetic field poorly represents the structural interpretation ofthe area. The northern border and most of the Atlantic coast show verylow gradients, with lower gradients trending towards the north and theeast. This partially substantiates a thickening of the non-magneticplatform deposits. The rest of the area contains some very highgradient, isolated and linear features. These features cannot becorrelated with present structural information and may be attributed tolithologic and/or structural complexities in the underlying Paleozoicand older basement material.-3-wbWAYCROSS0CORDELELAKE 8ACKSMEAR00 0 00 000 0 00 0 0 0000 00 00 4 o 0000MOULTRIE 00 00 0 0 0000"* 301300083 0000 00000 00000 0 0 0 000 00 00 0 46 o08040 0O Q 00 O 0 HAZLEHURSTOCMUL'.0 BAXLEY00 51 52 000 0 0434 3S436 041 o.000p po 00 0.. o.0080 0 00"7ow8 1.0::O - 0 0 888.8 88 88 817 ,1.0.0.o 9 0 0 080*0e$800 )TIFT0N00 0.000 0... . R VE:8.. 0_ 0 0 00 00 0080m ":8inS.o.0.00 0 00 0 0 o 00 00 0 0 80007 8 o~0...o.00 -00... .0 O - ;0"o -- . .00 000000 00 0DOUGLAS0 00 0o O o00o 021422200 00 0 0 0 00 Q0 000o14 15.0a .8 80 .0 000 000 0 4223 24 00000 00 a o 00 0 00RIVED0000 000000 0 0 0 0 0.0OKEFENOKEE SWAMP0310082 0084 00Figure 3 - Uranium Anomaly/Interpretation Map - Waycross Quadrangle.0000 _118031 30.0060 08 oS82 00DO.. ---I-]URANIUM ANOMALY/INTERPRETATION MAPWAYCROSS QUADRANGLEU.S. DEPARTMENT OF ENERGYAPPROXIMATE SCALE 1500,000EXPLANATION- CITY OR TOWN-URANIUM SAMPLE MEETING FOLLOWING CRITERIA(1) 1.010 U S(2) -1.0 5 T <_(3) 1.0 U/T SIN STANDARD DEVIATION UNITS.EACH SQUARE REPRESENTS 1 STANDARD DEVIATION.Od -URANIUM ANOMALY:A SINGLE SAMPLE OF 3 OR MORE STANDARDDEVIATIONS OR GROUP OF ADJOINING SAMPLESWHICH TOGETHER TOTAL 4 OR MORE STANDARDDEVIATIONS, 4.0 0sum S , WITH AT LEAST ONESAMPLE OF 2 OR MORE STANDARD DEVIATIONS.SURVEY ANDCOMPILATION BYGEGsG GECM1ETRICS2 6 0 00002/ WAYCROSS0 0 0 00 031 001 84 00 0BRUNSWICK12 i-4a -Figure 3a - Uranium Anomaly/Interpretation Map - Brunswick Quadranglewb310000 al 000020rGLENNVILLEFORT STEWART0 .00 0 o 0 O OLUDOWICI00 0 o <,o 00 0 0 0 0 00 o 000JESUP 4 y0 0 0 0 0 000000 00 016000-00 ATL NTIC OCEAN000 0 0SAI"BRUNSWICKNAIHUNTA 0 0 000 Q1004 5el 00 80 00- |32 00-1 331 00._.__80 00______URANIUM ANOMALY/INTERPRETATION MAPBRUNSWICK QUADRANGLEU.S. DEPARTMENT OF ENERGYAPPROXIMATE SCALE 1:500,000EXPLANATION- CITY OR TOWN- URANIUM SAMPLE MEETING FOLLOWING CRITERIAI1) 1.0 5 U S(2) -1.0 5 T So(3) 1.0 5 U/T S wIN STANDARD DEVIATION UNITS.EACH SQUAREDREPRESENTS 1 STANDARD DEVIATION.0 -URANIUM ANOMALY:A SINGLE SAMPLE OF 3 OR MORE STANDARDDEVIATIONS OR GROUP OF ADJOINING SAMPLESWHICH TOGETHER TOTAL 4 OR MORE STANDARDDEVIATIONS, 4.0 5 sum 5 -, WITH AT LEAST ONESAMPLE OF 2 OR MORE STANDARD DEVIATIONS.COMPILATION BYEGsG GEOMETRICS131 0BIBLIOGRAPHYAntoine, J. W., Martin, R. G.,1974, Continental Margins ofContinental Margins, Burke,683-694.Butler, A. P., Jr., Finch, W.genetic Uranium Deposits inSurvey Mineral Resources MapJr., Pyle, T. G.,the Gulf of Mexico:C. A., and Drake,and Bryant, W.R.,in The Geology ofC. L., (eds.), p.I., and Twenhofel, E. S.,the United States: U.S.MR-21, scale 1:3,000,000.1962, Epi-GeologicalMartel Laboratories, 1980, Geology of the Brunswick Quadrangle: scale1:250,000.Martel Laboratories, 1980, Geology of the Waycross Quadrangle: scale1:250,000.Murray, G.E., 1961,of North America.Geology of the Atlantic and Gulf Coastal ProvinceNew York: Harper and Row, 692 p.Puri H.S., and Vernon, R.O., 1964. Summary of the Geology of Floridaand A Guidebook to the Classic Exposures. Florida Geological SurveySpecial Publication No. 5 (Revised).Richards, H.G., 1975, United States - Atlantic Coastal Province: inThe Encyclopedia of World Regional Geology Part 1; R. W. Fairbridge,editor.Schnabel, R. W., 1955, The Uranium Deposits of the United States: U.S.Geological Survey Mineral Resources Appraisals Map MR2, scale1:5,000,000.United States Geological Survey and American Association ofGeologists, 1962, Tectonic Map of the United States:1:2,500,000.Petroleumscale-5-APPENDIX A - Data Acquisition, Processing, andInterpretation Methods- ,- . . _...,ii_ _ -. ?: .. .: -s, _ _ _ . - .-:<::. .. .,.a_. t::S'_-'i" .?' '1 r _S . r, un ;_'" _ i' , . -_ :."1"'^..Mi," +:r f",:P' iCyL 1'. +1 ' 1_ti^.-.. -. .- : . r . . -.-- ---INTRODUCTIONGeneralUnder the U.S. Department of Energy's (DoE), National Uranium ResourceEvaluation (NURE) Program, geoMetrics, Inc., conducted a high sensitiv-ity airborne radiometric and magnetic survey. The data collection andprocessing were conducted under requirements set forth in Bendix FieldEngineering Corporation specification 1200-C, dated February, 1979.The objectives of the (DoE)/NURE program, of which this project is asmall part, may be summarized as follows:"To develop and compile geologic and other informationwith which to assess the magnitude and distribution ofuranium resources and to determine areas favorable for theoccurrence of uranium in the United States." (DoE)As an integral part of the DoE/NURE Program, the National AirborneRadiometric Program is designed to provide cost effective, semiquan-titative reconnaissance radio element distribution information to aidin the assessment of regional distribution of uraniferous materialswithin the United States.All Airborne data collected by geoMetrics during the course of thisproject were done so utilizing a Beechcraft B65 Queen Air Airplane(U.S. Registry No. N9AG) and a Rockwell Aero Commander (Registry No.N1213B). Both aircraft used 3584 cubic inches of NaI crystal and a highsensitivity proton magnetometer (0.25 gamma).Each report contains a detailed geologic summary, interpretationreport, reduced scale copies of all maps and profiles, histograms, andstatistical tables for each quadrangle contained within the project.In addition, each report contains an appendix detailing the surveydescription, specifications, data collection and processing methods,and interpretation methods.All data processing, statistical analyses, and interpretation wereperformed at the geoMetrics computer facility, Sunnyvale, California.After processing, the corrected data were statistically evaluated todefine those areas which were radiometrically anomalous relative toother areas within each computer map unit. Standard deviation mapsand radiometric and magnetic profile data were first evaluated indivi-dually and then integrated into a final interpretation map for eachNTMS quadrangle.Corrected profiles of all radiometric variables (total count, potas-sium, uranium, thorium, uranium/thorium, uranium/potassium, and thorium/potassium, ratios), magnetic data, radar altimeter data, barometricaltimeter data, air temperature, and airborne bismuth contributions arepresented as profiles in this report. Single record and averaged dataare presented on microfiche in report. These data are given at 1.0second sample intervals, corrected for Compton Scatter, referenced to400 foot mean terrain clearance as Standard Temperature and Pressureand corrected for atmospheric bismuth. Digital magnetic tapes areavailable containing raw spectral data, single record data, magneticdata, and statistical analysis results.**Al**A2OPERATIONSPRODUCTION SUMMARYThe production summary presented below describes the general proceduresinvolved in gathering data for the entire project. The detailed dailyproduction summary in Appendix B describes a portion of the totalproject.Prior to the start of the survey operations, the airplanes were cali-brated at the DoE test pads and Dynamic Test Range (the Queen Air inApril 1980, and the Aero Commander in October 1980). Requirements forsystem calibrations are listed in the 1250-A specifications fromBFEC.Throughout the course of the overall project, the average groundspeed maintained by the Queen Air was 140 mph. The Aero Commanderaveraged 150 mph.Nearly 100% of the data collected were within the specificationlimits of 200-700 feet. Several deviations over short distances wererequired to meet military regulations, FAA safety requirements, and toensure that livestock were not endangered due to low flying aircraft.A sample altitude statistical distribution is shown in Figure I.0U-ULDATA COLLECTION PROCEDURESOperating Parameters/Sampling ProceduresThis survey was conducted using data collection parameters summarizedbelow:1. Data sampling was performed by a time-base system using 1.0 secondsample intervals. All sensor data with analog output were digit-ally sampled at each scan based upon the clock timing rate of 1.0seconds. The data so collected are the instantaneous values ofthe altimeter, temperature, pressure, and magnetometer parametersdetermined at the time of the data scan, but represent a counttime of 1.0 seconds for the gamma ray spectrometer data.********* '************************************************** ** ** ** * ** * ** * *** * ** * **** *** * *** * ** * * * *FIGURE ITypical Radar AltimeterStatistical SummaryHistogram for SingleFlight Line********************************************************* **** ** ** ** **** ** **** ** *1**r********************************* ** ** *** ** *2. The airplanes' objective ground speeds, mentionednot exceeded unless dictated by safety.3. The airplane's downward lookinginches providing an objective V/Vdivided by ground speed in milespreviously, werecrystal volume was 3,072 cubic(crystal volume in cubic inchesper hour) of 22.0 at 140 m.p.h.x ;ooco0r-qO etrLf l oL)r-'~- r,,a N ol 0C0000000ID5055N~0cC000000000000L Lr- 110 IDr-000.r-O t N N N - O O O O(000000000000000000000000D0Lr Ln0L)Lr L00 0 rrn rrr44. The upward looking crystal volume was 512 cubic inches.THE MINIMUM RADAR ALTMTR IS 147.500 FEETTHE MAXIMUM RADAR ALT"'TR IS 975.000 FEETTHE AVERAGE RADAR ALTXTR IS 424.336 FEETTHE STANDARD DEVIATION IS 123.4900 FEETZNWNavigation/Flight Path RecoveryFor all of the quadrangles, profiles were flown east-west at 6 mile(9.6 km) spacing. North-south tie lines were flown at 18 mile (28.8km) spacing.Navigation was accomplished using visual navigation techniques.Flight lines were drawn on 1:250,000 quadrangles and the pilot/navi-gator utilized these maps to provide visual navigation features.Simultaneously, a 35 mm tracking camera was used to record actualflight position. This camera's fiducial numbering system was directlysynchronized to the digital recording system such that a one-to-onecorrelation between position and data could be made. Upon completionof a data collection flight, the 35 mm film was processed and actualflight path positions located on the appropriate scale map sheets.Infield System CalibrationDue to the complex nature ofinterpretation, much emphasisthe data collection system.to ensure continuous high qualcalibration procedures used areboth the system and the required datawas placed on infield calibration ofThe objective of this calibration wasity of the data collected. The dailysummarized below:A. Pre Flight1. Use cesium sources (same positioning on crystals every day),peak each Photomultiplier tube/crystal using the digitalsplit-window detector of the GR-800. Then using thalliumsources, repeat the tuning of the individual crystals.2. Run full cesium spectrum onup looking crystals. Calcsample in Figure II). Rundown crystals for evaluationanalog recorder for both down andculate the cesium resolution (seespectrum out past the K40 peak onof system tuning.O O0t-- 4-)N 0.CD CD. LflQ 1c- C-)N..-01 4/mF-W.U-IV)UUOn0N0"r~0r--)0wna)..-3. Finally run a full thorium analog spectrum of the down crystalsand check for centering of K40 and T1208 peaks in spectrum.4. Repeat 1-3 until system is within contract specifications.B. During Flight1. Fly test line at survey altitude (400 ft), for approximatelyfive miles, prior to production data collection (record bothanalog and digital).2. Prioruated1of allto production data collection,to ensure +20% limits on totaltest flights from that base ofthe above data are eval-count compared to averageoperations.L),a)X >(1)3COXi7It!0I -.-- __{mm I17: 3.,...,. S _ ._ . -1......... ....y3~I ....... .__ ___2J. F00,. ... ...._ _ .'I . F_ __ ___. _.... ... _. . P . - ... ._. ..k. _._.___Vi ' _^_.......... _. _ , .. ........ .. i ... _.._....f .... i .. _ ._.- __--- -- T -- - -; _ .;- -_ _1.-_ _ _ _--_ _ _ -- --j0'1o 0w.0 u. v4- WCD t ..0 J-0-_1^ VeV_I.'-c l - _ _2..7 Ki -4rtE _ 3A3cc.'__}__...._ .. __ ............. _.._._._ wv._._fF3-1---_;__.._ijf-a... . . .. .e',1TTTTTT_. i4 - efzai**A4DATA COLLECTION SYSTEM3. During production data collection, monitor radon analog datafor unusual increases. Visually correlate these with tempera-ture and barometric pressure.4. Upon completion of production data collection, refly test lineat survey altitude (400 ft). Record both analog and digital.C. Post Flight1. Verify test line total count within 20% of average for alltest lines at that base of operations.2. Using cesiumcesium spectrerecord throughthe procedurewindow.sourcesum forh theusings (same position aboth down and upK40 peak in thecthallium sourcess pre-flight),crystals (aldown crystals).and examineAIRCRAFTTwo aircraft were used for this survey: (1) a Beechcraft Queen Air -Model 65 (U.S. Reg. No. N9AG), and (2) a Rockwell Aero Commander 680F(U.S. Reg. No. N1213B). Both these aircraft, being medium size withtwin engines, possess overall performance and safety features whichmake them ideal for low level, fixed-wing airborne geophysical surveysin areas of up to moderately high topographic relief. They can carryadequate payloads at low constant airspeeds, while maintaining economyand a wide envelope of safety. Performance data for the two craft intheir present survey configuration are given below.run fulllow it toRepeatthe T12083. Calculate the resolution of down and up crystal pack.4. Determine shift, if any, in T1208 peak position.Field Digital Data VerificationAt the completion of each flight, the raw digital data tapes werechecked for data quality and completeness on geoMetrics' G-725.The G-725 system is a totally portable mini computer (and peripherals)consisting of; an Interdata 516, two 9 track tape drives, a CRT,a line printer, and two floppy discs. Any digital problems encounteredwere immediately evaluated by the electronics operator and data man,thus assuring optimum data quality. In addition, histogram informationfor each measured variable was generated. Thus a summary displayof altitude, etc., is available for immediate evaluation.QUEEN AIRMaximum Aircraft Gross WeightAircraft Empty (dry)Max. useful load including fuelGeophysical PackageNavigation EquipmentFuel Tanks FullPilot & Electronics OperatorMin.SafeRateRateControl Speed at G.W. (IAS)Single Eng. Speed @ G.W. (IAS)of Climb 2 engines @ gross (FPM)of climb 1 engine @ gross (FPM)7,700 lbs.4,640 lbs.3,060 lbs.1,110 lbs.125 lbs.528 lbs.350 lbs.Total 2,113 lbs.951051,300210mphmphAEROCOMMANDER8,500 lbs.5,200 lbs.3,300 lbs1,110 lbs.125 lbs.1,338 lbs350 lbs.2,923 lbs.NGNG1,500250Avgas consumption (ga/hr) at 75% powerEndurance (75% power)Range (75% power - 45 min. reserve)366 hrs/6 mins.1,200 miles385 hrs/30 mins.1,100 milesCruise Configuration stalling speed at gross weight (IAS)0 bank450 bank80 mph95 mph80 mphNGElectronicsThe major components of the airborne data collection system aresummarized below (shown schematically in Figure III):1. Gamma Ray Spectrometer, geoMetrics GR-800, utilizing a dual256 channel capability to provide spectral data in the 0.4to 3.0 MeV range for both the downward looking and the upwardlooking crystal packages and coverage in the 3.0 to 6.0 MeVrange for cosmic background.2. Crystal Detector, geoMetrics Model DET-3072/512R consistingof 3072 cubic inches in the downward looking configurationand 512 cubic inches appropriately shielded in an upward lookingconfiguration.3. A geoMetrics Digital Data Acquisition System, Model G-714 with"read-after-write" data verification, recording the followingon magnetic tape:a. 512 channels of gamma ray spectrometer datab. Total magnetic intensityc. Fiducial number from data system/camerad. Manually inserted information, i.e. date, survey area,and flight line numbere. Altitude from radar altimeter and barometric altimeter(by analog-to-digital conversion)f. Time in days, hours, minutes and secondsg. Outside air temperature4. Magnetometer, geoMetrics Airborne Model G-803, capable of 0.125gamma sensitivity, but operated at 0.25 gamma sensitivity.5. Radar Altimeter, Bonzer Model Mark 10 with recording outputand display operating over an altitude range of 0 to 2,500 feet.6. Rosemont Barometric Altimeter with recording output and display.7. Recording Thermometer for monitoring outside air temperature.8.iiiiaofnlIitUJICIN0O2HN07OI FHn mIN0 mY'- Ya Yo Y0O = OO 1<-O6Owr O Q< Q0OII---LmCo-gyI II II II II II II II II I~iowU CZ CSI 2VTracking Camera. Automax 35 mm framing camera with wide anglelens and 10 character fiducial/line number display to provideflight path recovery data.-ooxU-xa.I (I II II I II IxoiiL _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ atl3gnnN 3NIIL_ - - _ _ _ _ _ _ _ _ _ - _ - - _ - _ - U838WnN IVIJnal3(N"S)3sind av3uA5VOaaO4OQ~QHQQc-0LLwLLKTHUNOtOLIHwIU')z0m1 IiiiiiiiJiiiiiiiiiiiiiiiiiiiiiiiiiiiiii.JiiiiiiiiiiiIIIIIIIIIIIIIL3SlOd HOIOW 3AWau< woac7OOazA6SYSTEM CALIBRATION9. Analog Recorder geoMetrics (MARS 6)to record the following data:a. Bi214 using a window about the 1.76 MeV peak from the down-ward looking system.b. Bi air background from the upwardlooking system.c. Magnetometerd. Radar Altitudee. Total count for downward looking system (0.4 to 3.0 MeV)f. Barometric Altitudeg. Time markers10. HP 7155 single channel analog recorder during pre and postflight calibrations, this recorder is used to plot a full analogspectra for both the down and up crystal systems via the GR-800.Thus, a hard copy record of the data used for resolution, drift,etc., checks are available at all times. This approach providesinstant verification of system parameters (refer to Figure II).AIRCRAFT AND COSMIC BACKGROUNDFull spectral data are collected at five (5) altitudes over water(14,000 feet, 12,000 feet; 10,000 feet; 8,000 feet and 6,000 feet)in an area where the existence of no airborne Bi214 can be assured(off shore over the Pacific Ocean). This results in separate spectraas shown schematically in Figure 10. We define S(12,000) to be thespectra at 12,000 feet from 0.4 MeV to 3.0 MeV with S(8,000) thesame spectra at a lower altitude (8,000) and C.(h) the total countbetween 3.0 and 6.0 MeV at respective altitudes.' Since the aircraftbackground is constant, the difference between any two altitudesseparated sufficiently - typically, 2,000 feet - yields the cosmicspectral curve shape as shown schematically in Figure VI. ThusS(12,000) - S(8,000) = ASandEC12 (hi) - Y C8 (hi) = ACThis cosmic spectral curve is scaled back to 12,000 feet as follows:C12 (hi) XASAC= A C (12,000) the Cosmic Spectrum (shape andmagnitude at 12,000 feet)The aircraft background is derived as follows:S(12,000) - C(12,000) = A/C BackgroundSince data were collected at five altitudes, this procedure wasrepeated for each combination of altitudes and results averaged.Typical aircraft and cosmic spectra are shown in Figures V, AND VIrespectively.SYSTEM CONSTANTSSystem constants were determined by occupation of the DoE WalkerField Test Pads. (See Ward, 1978, and Stromswold, 1978, for completedescriptions of the building and monitoring of the pads). The fivetest pads contained varying concentrations of K, U, and T as pre-sented by BFEC:S(12,o00)EC1I0 MeV 3 65(8,000)~C8Since the measurements were taken over a relatively short time period(a few hours), it was assumed that the matrix pad measurementscontain not only the effects of the matrix pad itself, but alsoaircraft background (which is a constant), cosmic background (cons-tant over the time period of interest), and all other local back-ground (e.g. BiAir, etc.) effects. (The matrix pad is constructedwith only the basic concrete mix without the additional elementalminerals). Thus, by subtracting the matrix pad count rates fromthe count rates in the four pads, we have eliminated aircraft andcosmic background and BiAir effects for the four pads. The padconcentrations are then modified in a similar fashion by the sub-traction of the matrix pad concentrations. The differential concen-trations in the pads are given in the table below.(hi)PADK-MatrixU-MatrixT-MatrixMixed-MatrixE?.-.AS = s(12,000) - s(8,000) AC3 6Considering the above, we can define a functional relationshipbetween the differential concentrations and the residual count rateswhich will provide a method of determining the calibration constantsfor the spectrometer system. These calibration constants are the six(6) stripping coefficients which account for the interactionsoccuring between the elemental channels in the system (Comptonscatter coefficients, etc.).On the basis of an ideal situation, one would anticipate that some ofthese interactions should be negligible. This is not totally thecase, since we are dealing with a system which has less than infiniteresolving power (i.e. the energies are smeared to some extent).FIGURE IV - Multiple altitude spectra schematic0-U2 (hi)PADMatrixA7KUTK1.45%5.14%2.03%2.01%4.11%U2.19 ppm5.09 ppm30.29 ppm5.14 ppm20.39 ppm0~MixedT6.26 ppm8.48 ppm9.19 ppm45.33 ppm17.52 ppm0 MeV 3 60UK3.7%0.6%0.6%2.7%0U2.9 ppm28.5 ppm3.0 ppm18.8 ppmT2.2 ppm2.9 ppm39.0 ppm11.3 ppmMeVti iL-DERIVED AIRCRAFT BACKGROUND SPECTRUM FROM PACIFIC OCEAN DATA AIRCRAFT BACKGROUNDDOWNWARD-LOOKING CRYSTAL SPECTRUM FOR LINE AC BCD, DATED 072577 ROTARY WING AIRCRAFTDOWNWARD LOOKING CRYSTALTC (0-6 MEV) 184.07 TC (0.4-3.0 MEV) 141.17 COSMIC (3-6 MEV 0.00 2048 CUBIC INCHESU (1.12 MEVI 9.91 K (1.46 MEV) 14.54 U (1.76 MEV) 4.36 T (2.62 MEV) 4.29 DMTE: 25 JULY 1977CM 6 (6.60 MEV) 0.000 CPS ICH 1 (0.012 MEV) .000 CPS BCH 2 (0.024 MEV) 0.000 CPS CH 3 (0.035 MEV) 0.000 CPS *CH 4 (0.047 MEV) 0.00 CPS *CH 5 (0.059 MEV) 0.000 CPS CM 6 (0.071 MEV) 0.000 CPS CH 7 (0.083 MEV) 0.000 CPS *CM 8 (0.095 MEV) 0.000 CPS *CM 9 (0.106 MEV) 0.000 CPS CM 10 (0.118 MEV) 0.000 CPS *CM 11 (0.130 MEV) 0.000 CPS *CH 12 (0.142 MEV) .666 CPSCH 13 (0.154 MEV) 0.000 CPS *CM 14 (0.165 MEV) 0.00 CPS CH 15 (0.177 MEV) 0.000 CPS CH 16 (0.189 MEV) 6.006 CPSCH 17 (0.201 MEV) 0.000 CPS CH 18 (0.213 MEV) -0.025 CPS CH 19 (0.225 MEV) -0.020 CPS CH 20 (0.236 MEV) 0.080 CPS CH 21 (0.248 MEV) 1.401 CPS BBBCH 22 (0.260 MEV) 3.792 CPS 582****CM 23 (0.272 MEV) 4.280 CPS **********CM 24 (0.284 MEV) 4.334 CPS BBB8BBBBBBBBCH 25 (0.295 MEV) 3.748 CPS 282B**.B**CH 26 (0.307 MEV) 3.897 CPS *#**S*B8BBBBCH 27 (0.319 MEV) 3.818 CPS BB**8 8#CH 28 (0.331 REV) 4.236 CPS B*** **B*CH 29 (0.343 MEV) 3.433 CPS *****B*B*BCH 30 (0.35 MEVI 2.996 CPS ********CH 31 (0.366 MEVI 2.559 CPS *** * *BCH 32 (0.378 MEV) 2.269 CPS **8B*CH 33 (0.390 MEV) 2.102 CPS 2#222#2CM 34 (0.402 MEVI 2.081 CPS ***** TOTAL COUNTCM 35 (0.414 MEV) 2.121 CPS B***2*CM 36 (0.426 MEVI 2.114 CPS *****BCH 37 (0.437 MEV) 1.976 CPS B*B*BCM 38 (0.449 MEV) 2.290 CPS *******BCH 39 (6.461 MEV) 2.188 CPS ********CH 40 (6.473 MEV) 2.226 CPS * **B**CM 41 (0.485 MEV) 1.983 CPS ****8*BCH 42 (0.496 MEV) 2.165 CPS ****CM 43 (0.508 MEV) 2.158 CPS *****CH 44 (0.620 MEV) 2.267 CPS *****BCH 45 (0.532 MEV) 2.217 CPS B*B*28CH 46 (0.544 MEV) 1.997 CPS ****CH 47 (0.556 MEVI 2.447 CPS 88***CM 48 (0.567 MEV) 2.540 CPS ** **BBCH 49 (0.579 MEV) 2.586 CPS 88#222CH 50 (0.591 MEV) 2.768 CPS ** ***CH 51 (0.603 MEV) 2.481 CP B.8***CH 52 (0.615 MEV) 2.372 CPS 888###CM 53 (0.626 REV) 1.866 CPS BBBBBCH 54 (0.638 MEV) 1.682 CPS **##ICH 55 (0.650 MEV) 1.661 CPS ******CH 56 (0.662 MEV) 1.480 CPS ****CH 57 (0.674 MEV) 1.474 CPS BBBB8CM 58 (0.686 MEV) 1.447 CPS BBBCH 59 (0.697 MEV) 1.431 CPS *****CM 60 (0.709 MEV) 1.476 CPS ****CM 61 (0.721 MEV) 1.453 CPS *#**8CH 62 (0.733 MEV) 1.467 CPS ****CM 63 (0.745 MEV) 1.579 CPS ******CM 64 (0.756 MEV) 1.497 CPS *****CH 65 (0.768 MEV) 1.548 CPS *t*CH 66 (0.780 MEV) 1.421 CPS ****CH 67 (0.792 MEV) 1.282 CPS ****CH 68 (0.804 MEV) 1.155 CPS **CH 69 (0.816 MEV) 1.246 CPS ****CH 70 (6.827 MEV) 1.245 CPS ***BCH 71 (0.839 MEV) 1.161 CPS ****CH 72 (0.851 MEV) 1.253 CPS *****CH 73 (0.863 MEV) 1.231 CPS *###CH 74 (0.875 MEV) 1.425 CPS ***CM 75 (0.887 MEV) 1.452 CPS *****CH 76 (0.898 MEV) 1.543 CPS ******CH 77 (0.910 MEV) 1.444 CPS ****BCH 78 (0.922 MEV) 1.364 CPS ****CH 79 (0.934 MEV) 1.289 CPS 8**CM 80 (0.946 MEV) 1.150 CPS 8*BBCH 81 (0.957 MEV) 1.144 CPS ****CH 82 (0.969 MEVI 1.085 CPS *BBCM 83 (0.981 REV) 1.061 CPS ****CH 84 (0.993 MEV) 0.941 CPS **8CH 85 (1.005 MEV) 0.919 CPS ***CH 86 (1.617 MEV) 0.822 CPS *5*CH 87 (1.028 MEVI 0.816 CPS *5*CM 88 (1.040 MEV) 0.853 CPS *5*CH 89 (1.052 MEV) 0.901 CPS *8B BISMUTH 214CH 90 (1.064 MEV) 0.822 CPS * *CH 91 (1.076 MEV) 0.867 CPS ****CH 92 (1.087 MEV) 0.968 CPS ***CM 93 (1.099 MEV) 0.851 CPS ****CH 94 (1.111 MEV) 0.905 CPS *B*CH 95 (1.123 MEV) 0.847 CPS B8CH 96 (1.135 MEV) 0.861 CPS ***CM 97 (1.147 MEV) 0.800 CPS * *CM 98 (1.158 MEV) 0.727 CPS ***CH 99 (1.170 MEV) 0.751 CPS 8CM 100 (1.182 MEV) 0.607 CPS * * BISMUTH 214CH 101 (1.194 MEV) 0.663 CPS ***CH 102 (1.206 MEV) 0.657 CPS * *CH 103 (1.217 MEV) 0.633 CPS ***CH 104 (1.229 MEV) 0.719 CPS *5*CH 105 (1.241 MEV) 0.671 CPS ***CM 106 (1.253 MEV) 0.475 CPS 8CH 107 (1.265 MEV) 0.601 CPS * *CM 108 (1.277 MEV) 0.661 CPS *8*CH 109 (1.288 MEV) 0.669 CPS 8CH 110 (1.300 MEV) 0.606 CPS ***CM 111 (1.312 MEVI 0.630 CPS ***CM 112 (1.324 MEV) 0.652 CPS *5*CH 113 (1.336 MEV) 0.644 CPS *5*CH 114 (1.347 MEV) 0.652 CPS * *CH 115 (1.359 MEV) 0.791 CPS 8CH 116 (1.371 MEVI 0.787 CPS *** POTASSIUM 40CM 117 (1.383 MEV) 0.834 CPS **CH 118 (1.395 MEV) 0.984 CPS ***CH 119 (1.407 MEV) 1.072 CPS ****CM 120 (1.418 MEV) 1.124 CPS ***CH 121 (1.430 MEV) 1.088 CPS ***CH 122 (1.442 MEV) 1.210 CPS *****CH 123 (1.454 MEV) 1.231 CPS 888CH 124 (1.466 MEVI 1.207 CPS ** *CH 125 (1.477 MV ) 0.995 CPS 88CH 126 (1.489 MEV) 0.967 CPS ***CH 127 (1.501 MEV) 0.624 CPS *5*CH 128 (1.513 MEV) 0.635 CPS 8CH 129 (1.525 MEV) 0.512 CPS ***CH 130 (1.537 MEVI 0.488 CPS 8CH 131 (1.548 MEV) 0.409 CPS 8CH 132 (1.560 MEV) 0.369 CPS ** POTASSIUM 40CH 133 (1.572 MEV) 0.339 CPS 8CH 134 (1.584 MEV) 0.438 CPS 8CH 135 (1.596 MEV) 6.310 CPS CM 136 (1.608 MEV) .259 CPS *CH 137 (1.619 MEV) 0.250 CPS 8CH 138 (1.631 MEV) 0.353 CPS *CH 139 (1.643 MEVI 0.323 CPS 8CH 140 (1.655 MEV) 0.332 CPS 8CM 141 (1.667 MEVI 0.326 CPS * BISMUTH 214CH 142 (1.678 MEV) 0.267 CPS 8CM 143 (1.690 MEV) 0.275 Cps 88CH 144 (1.702 MEV) 0.245 CPS 8CH 145 (1.714 MEV) 0.347 CPS 8CH 146 (1.726 MEVI 0.352 CPS 8CH 147 (1.738 MV6) 0.293 CPS 8CH 148 (1.749 MEVI 0.359 CPS *CH 149 (1.761 MEVI 6.270 CPS 8CM 150 (1.773 MEV) 0.334 CPS 88CH 151 (1.785 MEVI 0.245 CPS 8CM 152 (1.797 MEV) 0.255 CPS 8CH 153 (1.808 MEVI 0.174 CPS 8CH 154 (1.820 MEV) 0.228 CPS 8CH 155 (1.832 MEV) 0.18 CPS *8CH 156 (1.844 MEV) 0.115 CPS *CH 157 (1.856 MEV) 0.084 CPS * BISMUTH 214CH 158 (1.868 MEV) 0.147 CPS 8CH 159 (1.879 MEV) 0.147 CPSCH 160 (1.891 MV6) 0.139 CPSCH 161 (1.903 MEV) 0.109 CPS 8CM 162 (1.915 MEV) 0.091 CPSCM 163 (1.927 MEV) 0.151 CPSCH 164 (1.938 MV6) 0.088 CPSCM 165 (1.950 MV6) 0.136 CPSCH 166 (1.962 MV6) 0.157 CPS CH 167 (1.974 MV6) 0.119 CPSCM 168 (1.986 MEV) 0.109 CPSCH 169 (1.998 MEV) 0.113 CPSCM 170 (2.009 MEV) 0.106 CPSCM 171 (2.021 MV ) 0.147 CPS *CM 172 (2.033 MEV) 0.137 CPSCH 173 (2.045 MEV) 0.171 CPS *CM 174 (2.057 MEV) 0.154 CPSCH 175 (2.068 MEV) 0.108 CPSCM 176 (2.080 MEV) .162 CPS *CH 177 (2.092 MEV) 0.104 CPS *CM 178 (2.104 MV6) 0.138 Cps 8CH 179 (2.116 MV6) 0.137 CPSCH 180 (2.128 MEV) 0.119 CPS *CM 181 (2.139 MEVI 0.169 CPS 8CH 182 (2.151 MEV) 0.148 CPS *CH 183 (2.163 MEV) 0.101 CPS CH 184 (2.175 MEV) 0.114 CPSCH 185 (2.187 MEV) 0.088 CPS CH 186 (2.199 MEV) 0.101 CPS CH 187 (2.210 MEV) 0.085 CPS *CH 188 (2.222 MEVI 0.130 CPSCH 189 (2.234 MV6) 0.117 Cps 8CM 190 (2.246 MEV) 0.113 CPSCM 191 (2.258 MV6) 0.116 CPSCM 192 (2.269 MEV) 0.088 CPSCH 193 (2.281 MEV) 0.097 CPS *CM 194 (2.293 MCV) 0.095 CPS CH 195 (2.305 MEV) 0.087 CPS *CH 196 (2.317 MEV) 0.059 CPSCM 197 (2.329 MEV) 0.015 CPSCH 198 (2.340 MEV) 0.041 CPS *CH 199 (2.352 MEV) 0.070 CPS 8CM 200 (2.364 MV6) 0.087 CPSCH 201 (2.376 MEV) 0.085 CPS *CH 202 (2.388 MCV6) 0.84 CPSCM 203 (2.399 MCV) 0.064 CPSCM 204 (2.411 MEV) 0.123 CPS * THALLIUM 208CM 205 (2.423 MEV) 0.076 CPS *CM 206 (2.435 MEV) 0.116 CPS *CH 207 (2.447 MEV) 0.147 CPS *CH 208 (2.459 MEV) 0.108 CPS *CM 209 (2.470 MEV) 0.120 CPS *CH 210 (2.482 MEV) 0.092 CPS *CM 211 (2.494 MEV) 0.127 CPS *CM 212 (2.506 MEV) 0.169 CPS **CM 213 (2.518 MEV) 0.206 CPS **CH 214 (2.529 MEV) 0.262 CPS **CH 215 (2.541 MEV) 0.184 CPS **CM 216 (2.553 MEV) 0.206 CPS **CM 217 (2.565 MEV) 0.195 CPS **CH 218 (2.577 MEV) 0.173 CPS **CH 219 (2.589 MEV) 0.201 CPS **CH 220 (2.600 MEV) 0.329 CPS **CH 221 (2.612 MEV) 0.232 CPS **CM 222 (2.624 MEV) 0.187 CPS **CH 223 (2.636 MEV) 0.171 CPS **CH 224 (2.648 MEV) 0.177 CPS **CM 225 (2.660 MEV) 0.089 CPS *CH 226 (2.671 MEV) 0.122 CPS *CH 227 (2.683 MEV) 0.124 CPS *CH 228 (2.695 MEV) 0.131 CPS *CH 229 (2.707 MEV) 0.090 CPS *CH 230 (2.719 MEV) 0.027 CPS *CH 231 (2.736 MEV) 0.012 CPS *CH 232 (2.742 MEV) -0.026 CPS *CH 233 (2.754 MEV) -0.024 CPS *CH 234 (2.766 MEV) 0.038 CPS *CH 235 (2.778 MEV) 0.003 CPS *CM 236 (2.790 MEV) 0.060 CPS *CH 237 (2.801 MEV) 0.038 CPS * THALLIUM 208CH 238 (2.813 MEV) 0.023 CPS *CH 239 (2.825 MEV) 0.008 CP9 *CH 240 (2.837 MEV) 0.078 CPS *CH 241 (2.849 MEV) 0.027 CPS *CH 242 (2.860 MEV) 0.047 CPS *CH 243 (2.872 MEV) 0.039 CPS *CH 244 (2.884 MEV) 0,084 CPS *CH 245 (2.896 MEV) 0.025 CPS *CH 246 (2.908 MEV) 0.025 CPS *CH 247 (2.920 MEV) -0.015 CPS *CH 248 (2.931 MEV) 0.037 CPS *CM 249 (2.943 MEV) -0.005 CP *CM 250 (2.955 MEV) 0.042 CPS *CH 251 (2.967 MEV) 0.002.CPS *CH 252 (2.979 MEV) -0.018 CPS *CH 253 (2.990 MEV) 0.031 CPS *CH 254 (3.002 MEV) -0.106 CPS * TOTAL COUNTCM 255 (3.014 MEV) 0.000 CPS *00FIGURE VDERIVED COSMIC SPECTRUM FROM PACIFIC OCEAN DATA COSMIC SPECTRUMROTARY WING AIRCRAFTDOWNWARD-LOOKING CRYSTAL SPECTRUM FOR LINE COSMIC, DATED 072577 DOWNWARD LOOKING CRYSTALTC (0-6 MEV) 5275.09 TC (0.4-3.0 MEV) 3245.27 COSMIC (3-6 MEV) 1000.00 2048 CUBIC INCHESU (1.12 MEVI 165.91 K (1.46 MEV) 181.83 U (1.76 MEV) 157.56 T (2.62 MEV) 213.66 DATE: 25 JULY 1977CH 0 (0.000 MEV) 0.000 CPS *CH 1 (0.012 MEV) 0.000 CPS *CH 2 (0.024 MEV) 0.000 CPS *CH 3 (0.035 MEV) 0.000 CPS *CH 4 (0.047 MEV) 0.000 CPS *CH 5 (0.059 MEV) 0.000 CPS *CH 6 (0.071 MEV) 0.000 CPS *CM 7 (0.083 MEV) 0.000 CPS *CH 8 (0.095 MEV) 0.000 CPS *CH 9 (0.106 MEV) 0.000 CPS *CH 10 (0.118 MEV) 0.000 CPS *CH 11 (0.130 MEV) 0.000 CPS *CH 12 (0,142 MEV) 0.000 CPS *CH 13 (0.154 MEV) 0.000 CPS *CH 14 (0.165 MEV) 0.000 CPS *CH 15 (0.177 MEV) 0.000 CPS *CH 16 (0.189 MEV) 0.000 CPS *CH 17 (0.201 MEV) 0.000 CPS *CH 18 (0.213 MEV) 1.091 CPS 3*CH 19 (0.225 MEVI 1.313 CPS *3CH 20 (0.236 MEV) 2.226 CPS **3CH 21 (0.248 MEV) 26.345 CPS *********3********3******CH 22 (0.260 MEV) 89.243 CPS ****3*3****3******3**********33*33*****3333333*33***3**3**33:*333*z*3n***3*3***3CH 23 (0.272 MEV) 100.516 CPS***********************YY*********I*******#*I#***X*I**IY1#***#X#**********************CH 24 (0.284 MEV) 103.036 CPS*************************************** *** XX*IX*X**********X*********CH 25 (0.295 MEV) 94.423 CPS *************** 333*3#*3*33*3*********33*******3:*****5X***s*************zzCH 26 (0.307 MEV) 88.893 CPS ***************8*k************** ***********;*********%********##******S*****CH 27 (0.319 MEV) 85.032 CPS *************33**55****3*****333333333333****3**3*******:33**33***z******z****CH 28 (0.331 MEV) 80.528 CPS ***3***3**3**3* *************3********33*z*I#***#******* * *33*3*3**3**C3***CH 29 (0.343 MEV) 78.271 CPS *********** ***I**33**********3**3****3***********3**3******** *3****XCH 30 (0.355 MEV) 72.498 CPS *****333*3333Y***#**k*#*3***3**#*************3*3*3*33*3333******3nCH 31 (0.366 MEV) 74.934 CPS *333*83********************3****** ******33******5*3333****3**CH 32 (0.378 MEVI 65.560 CPS ***************3***3*******3************3********3*******3**33CH 33 (0.390 MEV) 65.966 CPS ****3****3******3*****3**33*33******** *****3*3**33***3**3**CH 34 (0.402 MEV) 63.189 CPS **33*3*************3*****xX***#888**3********** 3*33*3*3 TOTAL COUNTCH 3 (0.414 MEV) 62.880 CPS ***************3*****t***33*33*3*#****3*338***3*****3**CH 36 (0.426 MEV) 64.078 CPS ***3***************333**#****#8888**** *#**********3CH 37 (0.437 MEV) 67.602 CPS *****X*****3**3**************33*****3******333****3*****1***1CH 38 (0.449 MEV) 69.116 CPS **3******3*************************************************CH 39 (0.461 MEV) 76.972 CPS *****#****3**3*******Y*******3**************z*3*3*33*******:3**Y*3Y***CH 40 (0.473 MEV) 84.879 CPS ***************************** 3**s*3*3*z3***3k*****33**z****3383:3****CH 41 (0.485 MEV) 96.049 CPS ***************3**3**********#*****;Y***********z**x#***********z*3****3*:*z:*z*zYY****CH 42 (0.496 MEV) 94.167 CPS *************3**3*********3**3******3***3*3*3*3****z:*3****3*** 3***13*3z**z33zzCH 43 (0.508 MEV) 86.706 CPS ***3*************#*****************************************CH 44 (0.520 MEV) 68.016 CPS *33******3**3*****3**************************************n*****CH 45 (0.532 MEV) 48.444 CPS *3**333*3******33**3***********3**3**33CH 46 (0.544 MEV) 40.965 CPS **33**********3****33**%*****CH 47 (0.556 MEV) 30.512 CPS *************3**X*****3******CH 48 (0.567 MEV) 33.160 CPS ********3*3***33*333*333;**#***CH 49 (0.579 MEV) 31.892 CPS ********33*******33**3*****sCH 50 (0.591 MEV) 25.907 CPS **************************CH 51 (0.603 MEV) 30.781 CPS ***#*3*****3******3***********zCH 52 (0.615 MEV) 27.055 CPS ****3***3333**3*3*3*3****3CH 53 (0.626 MEV) 27.982 CP 3*********33*33*****#*#**3CH 54 (0.638 MEV) 25.776 CPS **3***3***3****3*********3CH 55 (0.650 MEV) 22.988 CPS *****************3****CH 56 (0.662 MEV) 27.787 CPS *****3***333*****3*********CH 57 (0.674 MEV) 25.274 CPS 1**3******3***3*3***#**CH 58 (0.686 MEV) 25.240 CPS 3******3*33333**3*****CH 59 (0.697 MEV) 23.489 CPS ****3**********3****CH 60 (0.709 MEV) 24.769 CPS ***********************CH 61 (0.721 MEV) 22.350 CPS *********************CH 62 (0.733 MEV) 22.242 CPS *3********************3CH 63 (0.745 MEV) 22.424 CPS ********************CH 64 (0.756 MEV) 22.234 CPS ******3***************CH 65 (0.768 MEV) 20.332 CPS ********************CH 66 (0.780 MEV) 18.821 CPS *******************CH 67 (0.792 MEV) 20.493 CPS ********************CH 68 (0.804 MEV) 19.339 CPS ******************CH 69 (0.816 MEV) 19.021 CPS ***********33******CH 70 (0.827 MEV) 17.949 CPS ***3**************CH 71 (0.839 MEV) 20.235 CPS ***********3*******CH 72 (0.851 MEV) 17.491 CPS *****************CH 73 (0.863 MEV) 18.370 CPS ******************CH 74 (0.875 MEV) 16.244 CPS **************CH 75 (0.887 MEV) 16.331 CPS ****************CH 76 (0.898 MEV) 17.519 CPS ****** *********CH 77 (0.910 MEV) 16.689 CPS *****************CH 78 (0.922 MEV) 17.150 CPS *3*************3*CH 79 (0.934 MEV) 19.230 CPS *************** 3CH 80 (0.946 MEV) 17.111 CPS *****************CH 81 (0.957 MEV) 16.248 CPS *****************CH 82 (0.969 MEV) 14.954 CPS **************CH 83 (0.981 MEV) 17.324 CPS 8****3******3**3CH 84 (0.993 MEV) 16.276 CPS ***************CH 85 (1.005 MEV) 14.813 CPS *333*3*********3CM 86 (1.017 MEV) 15.703 CPS *******#**3***CH 87 (1.028 MEV) 13.767 CPS **********3***CH 88 (1.040 MEV) 16.414 CPS *3***3*******CH 89 (1.052 MEV) 13.642 CPS ************** BISMUTH 214CH 90 (1.064 MEV) 13.624 CPS *3*3********3*CH 91 (1.076 MEV) 13.517 CPS **3*******33CM 92 (1.087 MEV) 13.700 CPS *****3*****3CH 93 (1.099 MEV) 14.633 CPS ****3****3***CH 94 (1.111 MEV) 14.303 CPS *3***********3*CH 95 (1.123 MEV) 13.766 CPS 3************zCM 96 (1.135 MEV) 14.949 CPS **************CM 97 (1.147 MEV) 13.503 CPS *3*********CH 98 (1.158 MEV) 13.481 CPS *3*****Y****CH 99 (1.170 MEV) 13.189 CPS *************CH 100 (1.182 MEV) 13.602 CPS *3*8 ***3***Y BISMUTH 214CH 101 (1.194 MEV) 12.965 CPS **************CH 102 (1.206 MEV) 12.538 CPS 3****33***3CH 103 (1.217 MEV) 14.001 CPS ******33******CH 104 (1.229 MEV) 11.346 CPS *838*3*3**YCM 105 (1.241 MEV) 11.113 CPS 3*3*x**#CM 106 (1.253 MEV) 13.669 CPS ***3****33***CH 107 (1.265 MEV) 11.910 CPS *3****#*#I#CH 108 (1.277 MEV) 12.345 CPS **3*3**3*3*3CH 109 (1.288 MEV) 10.736 CPS **#*2**3***CH 110 (1.300 MEV) 11.444 CPS *********#*3CM 111 (1.312 MEV) 11.433 CPS *3**3**33CH 112 (1.324 MEV) 11.927 CPS *3*3*3*3*33*CH 113 (1.336 MEV) 11.846 CP *3** 3*3*YYCH 114 (1.347 MEV) 11.896 CPS * x33* *#*3*3CH 115 (1.359 MEV) 11.470 CPS *3***3****CH 116 (1.371 MEV) 11.864 CPS ************* POTASSIUM 40CH 117 (1.383 MEV) 10.286 CPS **3**333*CH 118 (1.395 MEV) 18.084 CPS **3*****3*CH 119 (1.407 MEV) 9.642 CPS **3*****CH 120 (1.418 MEV) 11.778 CPS 3*3*33*3*3*3CH 121 (1.430 MEV) 12.635 CPS ****#*****XY*3CH 122 (1.442 MEV) 10.661 CPS **3*3***CH 123 (1.454 MEV) 9.140 CPS 6888#**3CH 124 (1.466 MEV) 11.144 CPS **3*****3CH 125 (1.477 MEV) 10.766 CPS * #*3*33*33CM 126 (1.489 MEV) 9.260 CPS 3**3**3*CH 127 (1.501 MEV) 11.961 CPS *****3*CH 128 (1.513 MEV) 10.296 CPS *3*******CH 129 (1.525 MEV) 10.900 CPS *333*3*** *CH 130 (1.537 MEV) 9.022 CPS **33*3CH 131 (1.548 MEV) 10.311 CPS 33*333333CH 132 (1.560 MEV) 16.151 CPS *33*33*3* POTASSIUM 40CH 133 (1.572 MEV) 9.361 CPS *********CH 134 (1.584 MEV) 8.753 CPS *8 333*3*3CH 135 (1.596 MEV) 11.176 CPS 3*3*3*3**CH 136 (1.608 MEV) 10.130 CPS **********CH 137 (1.619 MEV) 10.551 CPS ***3* 3***3CH 138 (1.631 MEV) 9.204 CPS *********CH 139 (1.643 MEV) 9.159 CPS **3*333*CH 140 (1.655 MEV) 8.738 CP5S ******3*CH 141 (1.667 MEV) 8.679 CPS ****3 BISMUTH 814CH 142 (1.678 MEV) 10.154 C6P 3*33*33*3*3CH 143 (1.690 MEV) 9.743 CPS *****3CH 144 (1.702 MEV) 9.453 CPS 338 3*2 *CH 145 (1.714 MEV) 9.418 CPS *33*333*CH 146 (1.726 MEV) 8.4285 CPS 6*3*9* #CH 147 (1.738 MEV) 9.263 CPS 322***8CH 148 (1.749 MEV) 9.653 CPS 33*3***33CH 149 (1.761 MEV) 9.412 CPS **3*8*#CH 150 (1.773 MEV) 9.019 CPS *33*33388CH 161 (1.785 MEV) 9.329 CPS 33*33*3*3CH 152 (1.797 MEV) 10.232 CPS 8*3*1*3X98OH 153 (1.808 MEV) 9.686 CPS *****#88*3CH 154 (1.820 MEV) 7.911 CPS *****333CH 155 (1.832 MEV) 8.104 CPS *#*3**3CH 156 (1.844 MEV) 9.602 CPS3*333*33CH 157 (1.856 MEV) 9.473 CPS 33#*212 2 BISMUTH 214CH 158 (1.868 MEV) 8.568 CPS *3*3*3328CH 159 (1.879 MEV) 8.105 CPS 3*3*388CH 160 (1.891 MEV) 8.014 CPS *#15x8#3CH 161 (1.903 MEV) 8.35 CPS * #33*33CH 162 (1.915 MEV) 8.759 CPS *3*3*****CH 163 (1.927 MEV) 6.994 CP *******CH 164 (1.938 MEV) 8.477 CPS **3*3*33CH 165 (1.950 MEV) 8.144 CPS 33*2 38#CM 166 (1.962 MEV) 7.798 CPS ***3*33CH 167 (1.974 MEV) 8.214 CPS 33#*33CH 168 (1.986 MEV 9.240 CPS ***33***3CH 169 (1.998 MEV) 7.945 CPS *3*33*8CH 170 (2.009 MEVI 7.615 CPS 88*333** *CH 171 (2.021 MEV) 6.816 CP *3**33CH 172 (2.033 MEV) 8.408 CPS **3*3*3CH 173 (2.045 MEV) 7.196 CPS 3333*3CH 174 (2.057 MEV) 7.231 CPS ***3****CM 175 (2.068 MEV) 7.473 CPS 3***3CH 176 (2.080 MEV) 9.062 CPS ***3*3*CH 177 (2.092 MEV) 8.116 CPS *8*****CM 178 (2.104 MEV) 8.235 CPS *3*****CH 179 (2.116 MEV) 7.653 CP *****3**CH 186 (2.128 MEV) 8.338 CPS **3*****CH 181 (2.139 MEV) 7.237 CPS **38CH 182 (2.151 MEV) 7.528 CPS *3**3*3CH 183 (2.163 MEV) 8.039 CPS ********CH 184 (2.175 MEVI 8.536 CPS 3*3****33CH 185 (2.187 MEV) 8.888 CPS 3*3***3*CM 186 (2.199 MEV) 7.485 CPS 33***882CH 187 (2.210 MEV) 8.211 CPS ***33CH 188 (2.222 MEV) 8.233 CPS ********CH 189 (2.234 MEV) 8.066 CPS **3* 33**CH 190 (2.246 MEV) 7.825 CPS **3***CH 191 (2.258 MEV) 7.062 CPS *******CH 192 (2.269 MEV) 8.435 CPS *3*33*3*3CH 193 (2.281 MEV) 7.440 CPS 6***#CH 194 (2.293 MEV) 7.686 CPS *********CH 195 (2.305 MEV) 7.110 CPS **33*3*CM 196 (2.317 MEV) 7.329 CPS **3*38CH 197 (2.329 MEV) 7.890 CPS *********CH 198 (2.340 MEV) 7.771 CPS *3333*3*CH 199 (2.352 MEV) 7.147 Cps ***3**CH 200 (2.364 MEV) 6.729 CPS * ******CH 201 (2.376 MEV) 6.264 CPS **3*32CM 202 (2.388 MEV) 6.318 CPS **#***CH 203 (2.399 MEV) 7.050 CPS *****CM 204 (2.411 MEV) 6.506 CPS *3**33 THALLIUM 208CH 205 (2.423 MEV) 6.486 CPS *33833CH 206 (2.435 MEV) 6.589 CPS ********CH 207 (2.447 MEV) 7.033 CPS ********CM 208 (2.459 MEV) 6.515 CPS ********CH 209 (2.470 MEV) 6.852 CPS ********CH 210 (2.482 MEV) 6.871 CPS ********CH 211 (2.494 MEV) 6.573 CPS *#******CH 212 (2.506 MEV) 6.417 CPS *******CH 213 (2.518 MEV) 5.845 CPS *******CH 214 (2.529 ME) 6.127 CPS *******CH 215 (2.541 MEV) 6.355 CPS *******CH 216 (2.553 MEV) 6.964 CPS ********CH 217 (2.565 MEV) 6.820 CPS ********CH 218 (2.577 MEV) 6.670 CPS *******CH 219 (2.589 MEV) 6.808 CPS ********CH 220 (2.600 MEV) 5.940 CPS ******CH 221 (2.612 MEV) 6.177 CPS *******CH 222 (2.624 MEV) 6.176 CPS *******CH 223 (2.636 MEV) 6.109 CPS *******CH 224 (2.648 MEV) 6.347 CPS *******CH 225 (2.660 MEV) 7.049 CPS ********CH 226 (2.671 MEV) 5.757 CPS *******CM 227 (2.683 MEV) 5.645 CPS *******CH 228 (2.695 MEV) 5.229 CPS ******CH 229 (2.707 MEV) 5.415 CPS ******CH 230 (2.719 MEV) 6.190 CPS *******CH 231 (2.730 ME) 6.092 CPS *******CH 232 (2.742 MEV) 6.466 CPS *******CH 233 (2.754 MEV) 7.032 CPS ********CH 234 (2.766 MEV) 5.533 CPS *******CH 235 (2.778 MEV) 6.309 CPS *******CH 236 (2.790 MEV) 5.559 CPS *******CH 237 (2.801 MEV) 5.206 CPS ****** THALLIUM 208CH 238 (2.813 MEV) 6.045 CPS *******CH 239 (2.825 MEV) 5.257 CPS ******CH 240 (2.837 MEV) 5.640 CPS ******CH 241 (2.849 MEV) 5.835 CPS *******CH 242 (2.860 MEV) 5.348 CPS ******CH 243 (2.872 MEV) 4.804 CPS *****3CH 244 (2.884 MEV) 4.742 CPS *#****CH 245 (2.896 MEV) 5.304 CPS ******CH 246 (2.908 MEV) 5.248 CPS ******CH 247 (2.920 MEV) 6.036 CPS *******CH 248 (2.931 MEV) 5.711 CPS *******CH 249 (2.943 MEV) 5.513 CPS *******CM 250 (2.955 MEV) 5.010 CPS ****CM 251 (2.967 MEV) 5.579 CPS *******CH 252 (2.979 MEV) 6.256 CPS *******CH 253 (2.990 MEV) 5.207 CPS ******CH 254 (3.002 MEV) 9.302 CPS ********** TOTAL COUNTCH 255 (3.014 MEV)1000.000 CPS ***##**************#*******#**********************************************************FIGURE VIThus, energy peaks within a spectrum of a given element are Gaussianshaped rather than pure line spectra. Additionally, we are dealingwith finite spectral windows, multiple peaked spectra, and pulsepileup; all tend to couple each window's response to the other.Keeping in mind that we are dealing with the count rates correspond-ing to the concentrations presented in the last table, we define thefollowing:where "i"KCi = uncorrected system count rate for the K channelUCi = uncorrected system count rate for the U channelTCi = uncorrected system count rate for the T channelKi = the percent differential concentration of potassiumUi = ppm differential concentration of uraniumTi = ppm differential concentration of thoriumrefers to the ith pad.KCkUCkTCkKCuUCuTCuT padSeparating theseuncorrected count(K pad)KCtUCtTCtequaratesKCk= CkkK + CkuU + CktT= CukK + uuU + CutT= CtkK + CtuU + cttT= ckkK + CkuU + CktT= CukK + CuuU + CutT= CtkK + CtuU + CttT= CkkK + CkuU + CktT= CukK + CuuU + CutT= ctkK + CtuU + CttTtion into consistent groups, we get for thein the K channel= tkkKk + zkuUk + CktTkWe also define the following:kk=C ku=C kt=Cuk=C uu=Sut=tk=C tu=C tt=sensitivity ofsensitivitysensitivitysensitivitysensitivitysensiti vi tysensitivitysensitivitysensitivityofofofofofofofofKCi toKCi toKCi toUC1 toUC1 toUC1 toTCi toTCi toTCi toUsing the above definitions,concentrationsconcentrationsconcentrationsconcentrationsconcentrationsconcentrationsconcentrationsconcentrationsconcentrationsof Kiof U1jof Tiof Kiof U1jof Tiof Kiof Ui1of Tiwe now construct the functional rela-tionship by means of the following nine (9) equations in sets ofthree (3) per pad.(U pad) KCu = r kkKu + kuUu + tktTu(T pad) KCt = ?kkKt + kuUt + CktTtThe equations can be expressed in matrix notationKCk Kk Uk Tkf kk]KCu = Ku Uu Tu - kuKCt Kt Ut Tt LCktWhere the k, u and t subscripts represent the K, U and T pads.In a similar manner we can write two other matrix equations forUCi and TCi respectively.UCk Kk Uk Tk BukUCu = Ku Uu Tu . uu[UCt Kt Ut TtbutAl0TCkTCTCtKk Uk= K UuKt UtTkT].TuTttkCtuOttCollecting the above, these equations can be expressed in matrixform asKCk UCk TCk Kt Uk Tk Ckk auk CtkKCu UCu TCu = Ku Uu Tu 'ku uu btuKCt UCt TCt Kt Ut Tt Ckt but OttKm = Akk(KCm + AhkUCm+ Akt TCm)Akk AkkUm 'u(UCm+ 6_t-TCm+ Auk KCm)Akk AuuTm= ktt(TCm+ AtUCm+ Atk KCm)Att EttThe terms in parentheses in the above 3 equations are the "correctedstripped count rates"are as follows:Sku = AkuAk kfor the system, and the stripping coefficients(effect of uranium on potassium)orA = B-where A is the residual count rate matrix, B is the matrix of theknown differential concentrations and C the sensitivity matrix.Rearranging the above equations we haveWe now define~ - =Skt = AktAk kSut AuAu uSuk A ukAuStu = AtuAttStk = AtkAttAEliminating c , we getB = AThese stripping coeffto eliminate confusionslightly differently.(effect of thorium on potassium)(effect of thorium on uranium)(effect of potassium on uranium)(effect of uranium on thorium)(effect of potassium on thorium)icients are defined in terms of Sij in orderwith a, , and y, which are sometimes definedWe can now solve for o by matrix inversion.Therefore, the differential concentrationsderived from the k,u,t pads to check the compKm Akk Aku AktUm = Auk Au Aut .Tm Atk Atu Attin the mixed pad can beuted Z.KCmUCmITCmIATMOSPHERIC RADON CORRECTIONConsider the crystal configuration shown below:Xtal 2a SA-Lead ShieldXtal 1where the subscript m refers to the mixed pad. Expanding this inalgebraic form we obtain the following set of equations:AllLLet 1 and 2 designate the down and up crystal respectively. The downcrystal sees radiation rates of I1 composed of the air signal Iand the ground signal I plus aircraft and cosmic background. agTherefore I1 = I9 + Ia + Al + C1Similarly, the up crystal sees the air signal and ground signal (bothsomewhat attenuated) plus an aircraft and cosmic background.Therefore I = QI2 g+ mI + A +Ca 2 2Where m is the response to the air signal andground signal getting through to the up detector.is the % of theUsing the test pad data, the factor can be determined. Considerthe two previous equations. When we subtract the matrix pad datafrom the K, U, and T pad data, we have essentially set A1 , A2 ,C ,and C and I equal to zero.1' 2 aTherefore I1I2= I= RIg(12I1Instead of using the count rates we can use the resultant sensitivi-ties 1/Auu to determine z for the elemental channel U.1/Auu (up)1/Auu (down)It should be noted that due to "shine around" (since the shielding isnot an infinite plane, the upward looking crystal responds to thesurrounding terrain) on the test pads, as altitude increases, shoulddecrease, thus Q= f(h).Only the factor m remains to be determined. This unfortunatelycannot be determined from test pad data. It can however be deter-mined by flying over water (e.g. use of the Lake Mead over-waterdata).Consider the equations for I1 and 12 againIi = Ig+ Ia + A + C12 = 'g + mIa + A2 + C2Over water Ig = 0We have A1 , A2, C1, and C2 defined.Removing the aircraft and cosmic background from the over water dataand we are left withI= IaI2 = mIaSince m is the shielding factor response to the air signal, we shouldhave an air signal to "shield". Thus m is best determined if thereis radon present.Both up and down counting rates are corrected for aircraft and cosmicbackground and so we can solve the following two equations for'a-'1 = Ig + Iabut12 =kAIg + mlamla = 12 - ElgIg= II - athen Ia (m-Q) = '2 - 1or Ia= 2- Elm - L= Bi Airand Ia is then the Bi Air contribution from the surrounding air.This is then subtracted from the down looking U count resulting incorrected data.A12DATA PROCESSINGDATA PREPARATIONThe following sections summarize the techniques used for reductionand processing of the airborne data collected by geoMetrics.Field Tape Verification and EditThe field data tapes containing the airborne data are read on acomputer to verify the recording and data quality. Data recovery isessentially 100% from the field tapes. During this phase, statis-tics are generated summarizing all the variables recorded for eachflight line. Simultaneously, the spectral peaks are evaluated forshifts using a centroid calculation and the particular window's peakchannel. The data are also checked for correct scan lengths andproper justification of data fields within each scan and and livetime calculations are made. During this process, the desired windowdata fields are extracted from each spectrum and rewritten as areformatted copy tape. (Portions of this operation were performed inthe field using the G-725 field computer system.)The reformatted raw data for each flight line (with aborted or un-necessary flight line data edited out) are then checked for consis-tency, data spikes, gradients, etc. Every correction suggested by thecomputer is evaluated by the data processing personnel prior to imple-mentation. Upon completion of the phase, the data on the output tapeare "clean" and ready for subsequent correction of the radiometrics andtieing of the magnetics.information. These flight lines are then overlain on the geologicbase map and each map unit is digitized such that each sample fallswithin a single unit. This resulting location information is thenmerged with the geophysicial data using the fiducial numbers ascommon reference.RADIOMETRIC DATA REDUCTIONReduction of the raw window data was carried out utilizing systemcalibration constants as derived from high altitude over water flights,Lake Mead Dynamic Test Range, and the Walker Field Test Pads. The datareduction sequence used is summarized in Figure VII. Processing of thedata was performed using the window energies given below:Total count - 0.4 to 3.0 MeVKU- 1.37 to 1.57 MeV- 1.66 to 1.87 MeV (downward looking system)Uup - 1.04 to 1.21 MeV and 1.65 to 2.42 MeV (upwardlooking system)T - 2.41 to 2.81 MeVCosmic - 3 to 6 MeV (downward and upward looking system)Aircraft and Cosmic background for the Queen Air/Aero Commander overthese windows are as follows:Flight Line LocationA single frame 35 mm camera is used for obtaining position recoveryinformation. The photo locations are spotted or transferred toa suitable base map and are digitized. The fiducial numbers of thespotted points along each line are entered during the digityingprocess. A computer program is used to check the consistency ofthese data using calculated intersections from tie line to tie lineand from traverse to traverse. This program allows easy detectionof entry errors as well as potential flight path recovery errors.A computer program then calculates the map location for each inter-section and the beginning and end of each line based on the fiducialnumbers and the control line/tie grid. A computer plot is made ofthese locations to check against the field plot and correct editingQUEEN AIRAircraft Cosmic*TC (cps) 152.04 2.3833K (cps)Udn(cps)U (cps)upT (cps)16.06 0.13226.50 0.10983.17 0.55403.42 0.1503AERO COMMANDERAircraft Cosmic*220.3718.8210.855.354.352.39150.13340.10820.59150.1513*Cosmic background values are in cps per 1.0 cps in the 3-6 MeVwindow.**Al3A14DATA PROCESSING FLOW DIAGRAMFIGURE VIIRaw FieldTapesData Recording Reformatted -Verification Dataand Summary TapeThis step performs thefollowing:- System Live time calculation-Centroid calculation ofK,U,T peaks stabilitydetermination- Compares window outputwith spectral sums overwindows- Checks for spiking, etc.- Produces Line basedstatistics and histogramsfor radar and barometeraltitude, air temperature,and gamma ray variables.FlightPathRecoveryMapsGamma Ray CorrectionsI 2.'.DearTimeCorrectWindow DataSubtractA/C andCosmicBackgroundStripData---Statistical5. AdequacyCalculation6 AltitudeCorrectioniiIMergeFlightI Path /GeologyDataandCorrected DataJRaw SpectralData TapesT-"DigitalDiurnalDataSingle SingleRecord RecordReduced Reduced Printer PlotData Data Contour MapsTapes ListingJ RemoveS Diurnal and ,SIGRFMagneticMagneticanData AncillaryTapes StackedProfilesStatisticalAnalysisTapesStatisticalSummaryT apeAveragedRecordData ListingStandard DeviiEdit Data (Anomaly) MeRemoveSpikesfRadiometricMultiple- ParameterStacked ProfilesRecalculateStatisticalAdequacyUraiuaAndlyAverageData Separate Databy GeologicTypeSHistograms- - StatisticalAnalysisSt an dardDev ia t ionProcessinggsnationlaps Uranium Anomaly/Interpretation MapFIELD OFFICE-0.L Ir.. lilI. CalculateDetermine RatiosRadon Correctionand apply toData--...-......--....-ProduceDigitize and Verify FihFlight FLinetPath BaseRecovery MapDigitize andGeologic 1 VerifyMapsGeologyCompton corrections to theconstants:down data were made using the following All radiometric data presented in the strip charts have been normal-ized to 400 feet mean terrain clearance at STP using the expression:The ij subscripts represent the influence.thw .the i window.onexp - u.AERO COMMANDER0.87170.14080.28770.0273.15760x PT(h - 400)where h is the height in feet, . is the appropriate altitude at-tenuation coefficient, P is in mm of Hg, and T is in degrees Kelvin.In cases where the altitude exceeds 1,000 feet, the correction co-efficients were limited to the 1,000 foot value.Bi Air calculations are made using the following expressions:SijSku5ktSutSukStuStk0.0of the jth windowU - (R + C'uk R + C'ut Rts)9up us C'uu ks C'uu sBiAir m -All parameters except for Sut are considered constantconsidered an altitude dependent paramenter utilizingexpression (after Grasty, 1975).its. Sut wasthe followingWhere Uup = count rate from upward detectorsQ = crystal coupling constant+ 0.0076h, where h is the altitude inhundreds of feet.Altitude attenuation coefficients used are defined as follows:ALTITUDE ATTENUATION COEFFICIENTSTC (per foot)K (per foot)U (per foot)T (per foot)QUEEN AIR0.0020110.0027400.0024790.002048AERO COMMANDER0.0016880.0028000.0025360.002102m = crystal geometric factorC'uk, C'ut, C'uu, = stripping coefficients relating down datato up dataRus = stripped uranium count rate - down systemRks = stripped potassium count rate - down systemRts = stripped thorium count rate - down systemThe numerical values for the constants Q, m, C'uk, and C'uu aregiven below:Q,mc'kCukC'uuC'utQUEEN AIR0.11010.5960.009470.071360.04636-0.000032u m -0.000192AERO COMMANDER0.08900.4450.009640.085620.05644-0.00019-0.000112QUEEN AIR0.84370.15840.27030.094530.0**A150.056140.0Sut= Sut0**A16uQ &y m are altitude dependent as follows:Q= Q- pt x h, where h is in feetm = m -um x h, where h is in feetThese Bi Air data are filtered and the filtered results are thenremoved on a point by point basis from the corrected uranium windowdata.The window data are then evaluated for statistical adequacy prior toaltitude correction to ensure they are significant within the contextof the anticipated errors in count statistics.Statistical Adequacy TestThe statistical adequacy test is made to determine whether thecorrected data sample is sufficiently greater than the "noise" torepresent the "signal" of interest.We can define three separate criteria for detection thresholds(ref. Currie, Analytical Chemistry, Volume 40, No. 3, March 1968)of which only one is directly applicable to our case; this is the"critical level". This is the level at which the decision is madethat a signal is "detected". We thus define this critical level asthat level at which the data are statistically adequate.Setting the actual levels in counts per second, "a priori " for eachelemental window is difficult at best since the full effect of allparameters affecting the counts is not known to a sufficient degreeof certainty. If the corrections to the data are a significantportion of the count rate, most of the error (exclusive of systematicerrors due to electronics, etc.) in the corrected data can be ascrib-ed to random errors within the applied corrections. The correctionsare basically the results of counting radioactive decay products (gammarays) and are therefore assumed to follow the classical Poisson distri-bution. The following assumptions concerning these corrections are:1. In the best case, the error in each correction is additive.2. The sum of these corrections also follows a Poisson distribu-tion.3. The uncertainty in the correction itself is equal to thesquare root of the correction applied..4. This uncertainty is directly reflected in the corrected singlerecord count rate.With these assumptions in mind, the criterion for determining thestatistical adequacy of a given data sample is defined as follows:"If a corrected single record data sample exceeds 1.5 times thesquare root of the summed correction applied to that datasample, then that data sample is statistically adequate."Since any calculation using statistically inadequate data (such asratios) is also inadequate, the adequacy of each element of thesingle sample record data is tested prior to the calculation. Thisis done during the course of the processing by retaining all correc-tions applied to each data sample and determining its adequacy asexplained above.Not only are the results of this statistical adequacy test used toinsure that calculated ratios will be meaningful but they are alsoutilized to determine the optimum interval over which the data shouldbe averaged (e.g. 5 seconds or 7 seconds, etc.) to improve the overalldata statistical adequacy In the case of this project, the resultingaveraging sample interval was 7 seconds.Conversion to Equivalent ppm and PercentAt this point the data are single record corrected samples in units ofcounts per second. These data are then converted to equivalent ppm(parts per million) uranium, thorium and percent potassium. Theconversion factors are the sensitivities derived from the Lake MeadDynamic Test Range data at 400 feet mean terrain clearance.RadioelementKUTEquivalentPercent/ppm1%K1 ppmeu1 ppmeTQueen AirCounts/Second91.510.46.4Aero CommanderCounts/Second96.39.26.7A17DATA PRESENTATIONGeneralMAGNETIC DATA REDUCTIONThe magnetic data reduction processes are: correction for diurnalvariation, tieing to a common magnetic datum, and subtraction of theregional magnetic field as defined by the International GeomagneticReference Field (IGRF). During data acquisition, the magnetic field ismonitored by a ground-based diurnal magnetometer that samples everyfour seconds at a sensitivity of one-quarter gamma. These data arerecorded on magnetic tape along with the time for synchronization withthe airborne data.The diurnal data are edited to keep only samples taken during flighttime and remove spikes and man-made magnetic events. After editing,these data are displayed in profile form to ensure that all correc-tions necessary have been made. Next, the data are synchronized intime with the airborne data, interpolated, and subtracted from theairborne magnetic data.The diurnally corrected magnetic data are then processed by a tieingprogram that compares the magnetic differences at intersections offlight lines and tie lines. This program calculates individual mag-netic field biases for each flight tie line based on tie line intersec-tions. This allows miss-ties to be minimized throughout the survey.These biases usually represent, after diurnal correction, systematicmagnetic changes caused by such things as heading error, changes inlocation of the ground-based magnetometer, or changes in the airborneequipment. The biases are manually evaluated and selectively applied.The majority of the data products are presented in this report.These include the uranium anomaly/interpretation maps and pseudo-contour maps of potassium, uranium, thorium, and magnetic data whichare integrated as part of the text in the interpretation section. Inaddition to these data, this report contains data presented in the formof radiometric profiles, flight path recovery maps, standard deviationmaps, and histograms. Microfiche data are contained in the back coverof each report. Data tapes are available separately.Radiometric ProfilesStacked profiles were prepared from the averaged data for each traverseand tie line. These stacked profiles, plotted at a linear scale of1:250,000, contain the following parameters: corrected Total Count,percent potassium, equivalent ppm uranium, equivalent ppm thorium,eU/eT, eU/%K, and eT/%K ratios, equivalent ppm Bi Air, radar altimeter,and magnetometer data. Each of the stacked profile sheets contains aplot of the flight path superimposed on a geologic strip map. Includedalong these profiles are the fiducial numbers which correspond toflight path position as displayed on the flight path recovery maps.Each of the stacked profiles represents the data contained on thespecific flight line within the boundaries of the specified NTMSQuadrangle sheet.Radiometric traces on the stacked profiles contain an indicator show-ing those data which are statistically inadequate. These statistical-ly inadequate data are marked by a small vertical tick at the samplelocation. The altitude profile has been limited in display to 1,000feet. A dashed line at the 700 foot level is presented to show thosedata which do not meet the altitude specifications. The verticalscale of each variable remains constant on all stacked profiles. Whenoverranging occurs, the trace is stepped and the step labeled showingthe actual value. A pictorial representation of such a steppingprofile is shown in Figure VIII. At the end of each stacked profile, astatistical summary of the minimum value, maximum value, mean, andstandard deviation for that variable is presented.This reportquadrangle,1:500,000.contains an equivalent setphotographically reducedof stacked profiles for eachto an approximate scale ofMAGNETIC PROFILESA set of profiles containing the magnetic data (corrected, with IGRFremoved), barometric altimeter data, radar altimeter data, diurnalmonitor data, and temperature data are available at a linear scale of1:250,000. Each of the stacked profiles contains a plot of theflight path superimposed on the geology over which the aircraft flew.Reduced scale (1:500,000) copies of these are presented in of thisreport.0 gammas MAGNETOMETER VALUE 100 gammas425004250042400FLIGHT PATH MAPSFor each of the NTMS quadrangle sheets covered by this survey, aflight path position map is available at a scale of 1:250,000. Theactual flight path has been superimposed on the geologic quadranglemaps. Flight lines and tie lines are annotated along with fiducialnumbers of located positions. Reduced scale (1:500,000) copiesof these can be found in this report.STANDARD DEVIATION MAPSGamma ray standard deviation maps have been prepared for each NTMSquadrangle included in this survey. The six maps generated representthe following parameters: percent potassium, equivalent ppm uranium,equivalent ppm thorium, and eU/eT, eU/%K and eT/%K ratios. The datacontained in each map represent only those data which are consideredstatistically adequate. This automatically excludes all data collectedover water or data which falls outside of altitude specifications(i.e. altitude greater than 700 and less than 200 feet). The symbolismof each of the six maps is identical. The center of each circlerepresents the central averaged sample since the data had been averagedover a 7 second interval. The small boxes adjacent to each of thecircles represents one standard deviation from the mean for thatspecific data sample. In order to determine whether the data shownare represented by positive or negative standard deviations, considereach map with north pointing away from the viewer. For east/westlines (traverse lines) positive standard deviations lie above or to thenorth of the traverse line with negative standard deviation below or tothe south. On the north/south lines (tie lines) positive standarddeviations are to the left of the viewer (west) with negative standarddeviations to the right (east).These maps were generated at a scale of 1:250,000 for each NTMS sheetand in addition, are presented in each report at a reduced scale ofapproximately 1:500,000.HISTOGRAMSComputer generated histograms, showing the equivalent ppm and percentdistributions for the three gamma ray emitters and their ratios mea-sured and calculated as a function of computer map unit are presentedin this report (See Figure IX). Information contained on these his-tograms includes the standard deviation as calculated about the arith-metic mean (or median), and the total number of samples from which thestatistics were derived.FIGURE VIII Plotter Step Value LabelingA18A19DATA LISTINGSSingle record reduced and averaged record (statistical analysis)data listings have been prepared on microfiche. The microfiche arecontained in each report. Each of the single record and averagedrecord data listings are presented for the data contained in a singlequadrangle. The data contained in the single record data listings aresummarized below:MAP UNIT : TS TOTAL NUMBER 7 6OF SAMPLES 17 6 1. Fiducial numberURANIUM 2. System/Quality (SAKUT) - The first digit identifies the systemused to collect the sample. The remaining digits define theresults of statistical adequacy testing for altitude, potassium,uranium, and thorium. A value of 0 indicated that the dataare statistically adequate. A value of 1 indicates that thedata are statistically inadequate. All data collected in excessof 700 feet and less than 200 feet are considered statisticallyinadequate.3. Time - time presented in hours, minutes, and seconds4. Altitude - altitude presented in feet above terrain5. LAT/LONG - Latitude and Longitude presented in terms of decimaldegrees6. Magnetic field expressed in residual gammas7. Geology - code representing geologic units8. %K, eU, eT - percent potassium, equivalent ppm of uranium andthorium9. eU/eTH, eU/%K, eTH/%K - calculated ratios of the three parameters10. Total count - corrected total count data (0.4 to 3.0 MeV)11. COS - downward looking cosmic count rate in the 3-6 MeV channel12. Uair - atmospheric Bi-214 equivalent ppm13. Temperature - outside air temperature in degrees centigrade812}UU0ADEQUATE2. 8 17 481DAMPLESSample Computer Map Unit Histogram14. Press - barometric pressure in mm of mercuryi- 70hEAR /MEDIANEQUIVALENT PPM2.8FIGURE IX8.0The averaged record (statistical analysis) data listings are summar-ized below:1. Fiducial numberDATA INTERPRETATION METHODSGeneral2. System/Quality (SAKUT) - The first digit identifies the systemused to collect the sample. The remaining digits define theresults of statistical adequacy testing for altitude, potassium,uranium, and thorium. A value of 0 indicated that the dataare statistically adequate. A value of 1 indicates that thedata are statistically inadequate. All data collected in excessof 700 feet and less than 200 feet are considered statisticallyinadequate.3. LAT/LONG - Latitude and longitude presented in terms of decimaldegrees4. Magnetic field expressed in residual gammas5. Geology - code representing geologic formations6. %K, eU, eT - percent potassium, equivalent ppm of uranium andthorium data and the number of (+) standard deviations fromthe mean7. eU/eTH, eU/%K, eTh/%K - calculated ratios of the three parameters,and the number of (+) standard deviations from the mean8. Total count - corrected total count data (0.4 to 3.0 MeV)9. COS - downward looking cosmic count rate in the 3-6 MeV channel10. Uair - atmospheric Bi-214 in equivalent ppmDATA TAPESData tape files have been generated for each of the 1:250,000 NTMSquadrangle sheets. The tapes are IBM compatible and recorded on9 track EBCDIC at 800 bpi. Five separate types of data tapes arepresented: raw spectral data tapes, single record reduced data tapes,statistical analysis tapes, magnetic data tapes and a statisticalanalysis summary tape. Detailed descriptions of the data tape formatsfollow this discussion.The stated objective of the NURE Program is the evaluation of theuranium potential of the United States. In support of this goal,high sensitivity airborne radiometric and magnetic surveys have beenimplemented to obtain reconnaissance information pertaining to regionaldistribution of uraniferous materials. Within this context, datainterpretation has been oriented toward regional detection and descrip-tion of anomalously high concentrations of uranium.By far the most significant natural sources of gamma radiation inthe geologic environment are the radioactive decay series of potassium40 (K40), thorium 232 (Th232) and uranium 238 (U238) of which 0.7%is uranium 235. Potassium 40 is the largest contributor to naturalradioactivity, accounting for nearly 98%, as it is the most abundantgamma ray emitter-.012% of all potassium in nature. (Refer to GSAMemoir 97 for abundances of uranium, thorium, and potassium).Potassium 40 is directly identified by the airborne spectrometerfrom a single clear peak at 1.46 mev (million electron volts) in itsgamma ray spectrum. However, thorium 232 and uranium 238 do not haveany clear, distinct peaks at sufficiently high energies to allowdirect detection from airborne systems. Instead, daughter productswhich do have distinct peaks are measured as representing the abundanceof the parent element. For thorium 232, the daughter nuclide thallium208 (T1208) has a distinct peak at 2.62 meV while uranium 238 has adaughter, bismuth 214 (Bi214) possessing a clear peak at 1.76 meV(see Figure 7 for a composite decay series spectrum). Consequentlythe fundamental assumption implicit to airborne uranium and thoriummeasurements is that the measured daughter products are in radioactiveequilibrium - the number of atoms of disintegrating daughter nuclidesare equal to the number being formed (see Adams and Gasparini, 1970).An airborne gamma ray measurement is the sum of photons counted duringa specified time interval from a multitude of gamma ray sources whichinclude the three geologic emitters that are being sought plus otherinterfering sources. These others include, but are not limited tohigher energy cosmic rays, aircraft and instruments, contributionsfrom overlapping decay series and airborne radon 222. (See Burson,1974 and McSharry, 1973 for a more complete discussion of airborneradiometric measurements, and Radiometric Data Reduction in thisvolume for a complete description of data correction procedures).When correlating ground data (geochemical, geological, etc.) withthe corrected data derived from raw airborne measurements, the inter-preter must remember what an individual airborne gamma ray samplephysically measures. First, the terrestrial component of the gammaradiation measured by the airborne detector emanated primarily fromthe upper 18 inches of material on the earth's surface (Gregory andA20Horwood, 1963). The airborne measurement cannot "see" any deeperinto the underlying rock material and is essentially a measurementof the soil's or exposed (weathered) rock's radioactivity. Secondly,since each airborne sample is an accumulation of gamma rays measuredon a moving platform over a fixed period of time, the individualsample represents a large areal extent of surficial material. Forthis survey, with specifications of 400 feet mean terrain clearanceand an average ground speed of 140 miles per hour, a one second samplecorresponds to an oval approximately 750 feet long by 600 feet wide(assuming an infinite, uniformly distributed source). Accordingly,averaged samples represent tremendous volumes of surficial materials.MethodologyAs described previously, the gamma ray data were located by computermap units, histograms were produced and statistical analyses per-formed. The basic unit for interpretation then is the averaged sampleand its attendant deviations about a particular map unit's mean.The uranium anomaly/interpretation map displays each individualaveraged sample that meets the following criteria:1. The averaged uranium sample must be greater than or equal to1 standard deviation above its map unit mean.2. The sample must have a U/T ratio greater than or equal to 1standard deviation above its unit mean.3. Each U/T ratio defined in (2) must have a corresponding thoriumvalue lying at least greater than minus one (-1) standard devia-tion below the mean. If the thorium sample is less than onestandard deviation below the mean, the U/T ratio is consideredquestionable.All the possible anomalies displayed on the map are then examinedfor clusters, trends, and comparisons with all other available data.Minimum requirements in the subsequent interpretation discussions ofeach quadrangle for anomalies listed in the uranium anomaly summaryare defined as follows:Two (2) consecutive averaged U samples lying two or more stan-dard deviations above the mean or three (3) consecutive averagedU samples, two of which are one (1) or more standard deviationsand the third of which is two (2) or more standard deviationsabove the mean.Statistical anomalies which meet the above criteria can result fromseveral factors or circumstances including: (1) true concentrationof uraniferous minerals, (2) differential surface cover (soils and/orvegetation) within a lithologic unit, (3) local weather conditionssuch as rain and snow, (4) extreme facies variation within a mappedunit, and (5) differential weathering of rocks within mapped units.Obviously an averaged sample which lies on the boundary between twomap units is not truly reflecting either one, but is rather an averageof both. Thus, for two markedly different units', such a sample wouldbe anomalous relative to one of the units and not be a true indicationof radioactive differences within the unit.The percent potassium, equivalent ppm thorium and uranium, the threeratios and residual magnetic data were plotted as separate pseudo-contour maps and overlain on the geologic base map and standard devia-tion maps. Regional trends of each variable and average valves couldthus be easily and quickly determined and compared with the associatedgeological, magnetic, and statistical trends. Only the long wave-lengths within each variable would show any line-to-line continuityon the pseudo-contour maps and thus, only regional trends will appear.Each quadrangle's stacked profiles were also overlain on the corres-ponding geologic and standard deviation maps and anomaly map to furtherdelineate trends and to allow a more detailed analysis of individualanomalies. Since the interpretation was concentrated on detectionof anomalous uranium, subtle trends present in the potassium andthorium channels and ratios were only examined in a cursory manner.Even during such a brief examination of the profiles, it was evidentthat the spectrometer system was highly sensitive to changes in surfacematerials even in areas of low counting rates such as glacial drift.Thus radiometrics have a real potential for performing general sur-ficial mapping "geochemical analysis" on a geologic unit (or soils)basis in addition to merely radioactive mineral "anomaly hunting".A21TAPE FORMATS ITEM FORMAT DESCRIPTIONSINGLE RECORD REDUCED DATA TAPE 1314REFERENCE: Paragraphs 4.7.6 and 6.1.6, BFEC 1200-CThe Single Record Tape is an unlabeled, nine track, 800 BPI, NRZI.All data are recorded as EBCDIC characters. Each tape contains butone file of format, header, data, and trailer records for no morethan one quadrangle. The tape is divided into 6900-character blockscontaining the following information.Block 1 - Format DataThis block contains 6768 characters in 94 consecutive linescharacters containing the following literal description.02 0978 (DATA TAPE TYPE AND FORMAT SPECIFICATION DATE CODES)SINGLE RECORD REDUCED DATA TAPEFORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK)ITEM FORMAT1. A402. A203. 144. I15. I16. A207. F6.18. F6.19. F6.1DESCRIPTION131315-24 (SAME)* ** ** *NUMBER OF CHANNELS (0-3 MEV) INFIRST AERIAL SYSTEMNUMBER OF CHANNELS (0-3 MEV) INFIRST AERIAL SYSTEMREPEAT OF ITEMS 5-14 FOR SECOND***4PI SYSTEM FOR2PI SYSTEM FORAERIAL SYSTEM85-94 (SAME) REPEAT OF ITEMS 5-14 FOR NINTH AERIAL SYSTEM95 13 NUMBER OF FLIGHT LINES ON THIS TAPE96 14 FIRST FLIGHT LINE NUMBER ON THIS TAPE97 16 FIRST RECORD NUMBER OF FIRST FLIGHT LINE98 13 JULIAN DATE (DAY OF YEAR) FIRST FLIGHT-LINE DATAWAS COLLECTED99-101 I4,I6,I3 REPEAT OF ITEMS 96-98 FOR SECOND FLIGHT LINE ONTHIS TAPEof 72*********390-392 14,16,13 REPEAT OF ITEMS 96-98 FOR 99th FLIGHT LINE ONTHIS TAPEFORMAT FOR SINGLE RECORD REDUCED DATA RECORD (THIRD THRU LAST BLOCK)ITEMQUADRANGLE NAME AS PROJECT IDENTIFICATIONNAME OF SUBCONTRACTORAPPROXIMATE DATE OF SURVEY (MONTH, YEAR)NUMBER OF AERIAL SYSTEMS USED TO COLLECTTHIS QUADRANGLE12345678DATA FORAERIAL SYSTEM IDENTIFICATION CODE FOR FIRSTSYSTEMAIRCRAFT IDENTIFICATION BY TYPE AND FAA NUMBERFOR FIRST SYSTEMNOMINAL ALTITUDE SYSTEM SENSITIVITYTERRESTRIAL POTASSIUM (K-40) TO ONEIN CPS PER PERCENT KNOMINAL ALTITUDE SYSTEM SENSITIVITYTERRESTRIAL URANIUM (BI-214) TO ONEIN CPS PER PPM EQUIVALENT URELATIVE TODECIMAL PLACERELATIVE TODECIMAL PLACE910111213141516FORMATI1141616F8.4F8. 4F6.1F7.1A814F6.1F4.1F6.1F4.1F6.1F4.1NOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL THORIUM (TL-208) TO ONE DECIMAL PLACEIN CPS PER PPM EQUIVALENT THDESCRIPTIONAERIAL SYSTEM IDENTIFICATION CODEFLIGHT LINE NUMBERRECORD IDENTIFICATION NUMBERGMT TIME OF DAY (HHMMSS)LATITUDE TO FOUR DECIMAL PLACES IN DEGREESLONGITUDE TO FOUR DECIMAL PLACES IN DEGREESTERRAIN CLEARANCE TO ONE DECIMAL PLACE IN METERSRESIDUAL (IGRF REMOVED) MAGNETIC FIELD INTENSITYTO ONE DECIMAL PLACE IN GAMMASSURFACE GEOLOGIC MAP UNIT CODEQUALITY FLAG CODESAPPARENT CONCENTRATION OF TERRESTRIAL POTASSIUM(K-40) TO ONE DECIMAL PLACE IN PPM EQUIVALENT UUNCERTAINTY IN TERRESTRIAL POTASSIUM TO ONE DECIMALPLACE IN PERCENT KAPPARENT CONCENTRATION OF TERRESTRIAL URANIUM(BI-214) TO ONE DECIMAL PLACE IN PPM EQUIVALENT UUNCERTAINTY IN TERRESTRIAL URANIUM TO ONE DECIMALPLACE IN PPM EQUIVALENT UAPPARENT CONCENTRATION OF TERRESTRIAL THORIUM(TL-208) TO ONE DECIMAL PLACE IN PPM EQUIVALENT THUNCERTAINTY IN TERRESTRIAL THORIUM TO ONE DECIMALPLACE IN PPM EQUIVALENT TH*A22L*A23ITEM FORMAT DESCRIPTION17 F6.1 URANIUM-TO-THORIUM RATIO TO ONE DECIMAL PLACE INPPM EQUIVALENT U PER PPM EQUIVALENT TH18 F6.1 URANIUM-TO-POTASSIUM RATIO TO ONE DECIMAL PLACE INPPM EQUIVALENT U PER PERCENT K19 F5.1 THORIUM-TO-POTASSIUM RATIO TO ONE DECIMAL PLACE INPPM EQUIVALENT TH PER PERCENT K20 F8.1 GROSS GAMMA (0.4-3.0 MEV) COUNT RATE TO ONEDECIMAL PLACE IN COUNTS PER SECOND21 F6.1 UNCERTAINTY IN GROSS GAMMA COUNT RATE TO ONEDECIMAL PLACE IN COUNTS PER SECOND22 F5.1 ATMOSPHERIC BI-214 4PI CORRECTION TO ONE DECIMALPLACE IN PPM EQUIVALENT U23 F4.1 UNCERTAINTY IN ATMOSPHERIC BI-214 4PI CORRECTIONTO ONE DECIMAL PLACE IN PPM EQUIVALENT U24 F4.1 OUTSIDE AIR TEMPERATURE TO ONE DECIMAL PLACE INDEGREES CELSIUS25 F5.1 OUTSIDE AIR PRESSURE TO ONE DECIMAL PLACE IN MMHGThis description serves to identify the format of data on subsequentblocks on the tape. The remaining 132 characters on this block areblanks.STATISTICAL ANALYSIS TAPEREFERENCE: Paragraphs 4.7.7 and 6.1.6, BFEC 1200-CThe statistical analysis data tape is an unlabeled, nine track, 800BPI, NRZI. All data is recorded as EBCDIC characters. The blocklength is 8000 characters long. Each tape contains one file of datafor no more than one quadrangle.Block 1 - Format Description DataThe first physical block on this tape contains a format description fordata on subsequent blocks. The first 7560 characters on this blockcontains 105 lines of 72 characters exactly as written below:03 0978 (DATA TAPE TYPE AND FORMAT SPECIFICATION DATE CODES)STATISTICAL ANALYSIS DATA TAPEFORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK)ITEMBlock 2 - Single Record Reduced Identification DataThe second block contains the identifier information for the datacontained in subsequent blocks. The identification information iswritten according to the format description in the first half of thefirst block. The remaining 4978 characters on this block are blanks.12345Block 3 - Single Record Reduced DataThese blocks contain data written according to the format descriptionin the second half of the first block. There will be 50 logicalrecords per physical block. As of August 1979, the method for deter-mining uncertainties specified in the data blocks remains undefined,and those values are filled with 9's under format control.67891011121314FORMATA40A2014I1I1A20F6.1F6.1F6.116F6.3F6.31313DESCRIPTIONQUADRANGLE NAME AS PROJECT IDENTIFICATIONNAME OF SUBCONTRACTORAPPROXIMATE DATE OF SURVEY (MONTH, YEAR)NUMBER OF AERIAL SYSTEMS USED TO COLLECT DATA FORTHIS QUADRANGLEAERIAL SYSTEM IDENTIFICATION CODE FOR FIRSTSYSTEMAIRCRAFT IDENTIFICATION BY TYPE AND FAA NUMBERFOR FIRST SYSTEMNOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL POTASSIUM (K-40) TO ONE DECIMAL PLACEIN CPS PER PERCENT KNOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL URANIUM (BI-214) TO ONE DECIMAL PLACEIN CPS PER PPM EQUIVALENT UNOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL THORIUM (TL-208) TO ONE DECIMAL PLACEIN CPS PER PPM EQUIVALENT THBLANK FIELD (99999)4PI-SYSTEM DATA COLLECTION INTERVAL TO THREEDECIMAL PLACES IN SECONDS FOR FIRST SYSTEM2PI-SYSTEM DATA COLLECTION INTERVAL TO THREEDECIMAL PLACES IN SECONDS FOR FIRST SYSTEMNUMBER OF CHANNELS (0-3 MEV) IN 4PI SYSTEM FORFIRST AERIAL SYSTEMNUMBER OF CHANNELS (0-3 MEV) IN 2PI SYSTEM FORFIRST AERIAL SYSTEMFORMAT(SAME)*DESCRIPTIONREPEAT OF ITEMS 5-14 FOR SECOND AERIAL SYSTEM** * *85-94 (SAME) REPEAT OF ITEMS 5-14 FOR NINTH AERIAL SYSTEM95 13 NUMBER OF FLIGHT LINES ON THIS TAPE96 14 FIRST FLIGHT LINE NUMBER ON THIS TAPE97 16 FIRST RECORD NUMBER OF FIRST FLIGHT LINE98 13 JULIAN DATE (DAY OF YEAR) FIRST FLIGHT-LINE DATAWAS COLLECTED99-101 14,16,13 REPEAT OF ITEMS 96-98 FOR SECOND FLIGHT LINE ONTHIS TAPE***ITEMITEM15-24*390-392 14,16,13 REPEAT OF ITEMS 96-98 FOR 99th FLIGHT LINE ONTHIS TAPEFORMAT FOR STATISTICAL ANALYSIS DATA RECORD (THIRD THRU LAST BLOCK)FORMAT DESCRIPTIONAERIAL SYSTEM IDENTIFICATION CODEFLIGHT LINE NUMBERRECORD IDENTIFICATION NUMBERGMT TIME OF DAY (HHMMSS)LATITUDE TO FOUR DECIMAL PLACES IN DEGREESLONGITUDE TO FOUR DECIMAL PLACES IN DEGREESTERRAIN CLEARANCE TO ONE DECIMAL PLACE IN METERSRESIDUAL (IGRF Removed) MAGNETIC FIELD INTENSITYTO ONE DECIMAL PLACE IN GAMMASSURFACE GEOLOGIC MAP UNIT CODEQUALITY FLAG CODESAPPARENT CONCENTRATION OF TERRESTRIAL POTASSIUM(K-40) TO ONE DECIMAL PLACE IN PERCENT KUNCERTAINTY IN TERRESTRIAL POTASSIUM TO ONEDECIMAL PLACE IN PERCENT KPOTASSIUM STANDARD DEVIATION FROM THE MEAN TO ONEDECIMAL PLACE AND ALGEBRAICALLY SIGNEDAVERAGED CONCENTRATION OF TERRESTRIAL URANIUM(BI-214) TO ONE DECIMAL PLACE IN PPM EQUIVALENTUUNCERTAINTY IN TERRESTRIAL URANIUM TO ONE DECIMALPLACE IN PPM EQUIVALENT UURANIUM STANDARD DEVIATION FROM THE MEAN TO ONEDECIMAL PLACE AND ALGEBRAICALLY SIGNEDAVERAGED CONCENTRATION OF TERRESTRIAL THORIUM(TL-208) TO ONE DECIMAL PLACE IN PPM EQUIVALENTTHUNCERTAINTY IN TERRESTRIAL THORIUM TO ONE DECIMALPLACE IN PPM EQUIVALENT THTHORIUM STANDARD DEVIATION FROM THE MEAN TO ONEDECIMAL PLACE AND ALGEBRIACALLY SIGNED.FORMATF8.1F6.1F5.1F4.1F4.1F5.12021222324252627D829DESCRIPTIONGROSS GAMMA (0.4-3.0 MEV) COUNT RATE TO ONEDECIMAL PLACE IN COUNTS PER SECONDUNCERTAINTY IN GROSS GAMMA COUNT RATE TO ONEDECIMAL PLACE IN COUNTS PER SECONDATMOSPHERIC BI-214 4PI CORRECTION TO ONE DECIMALPLACE IN PPM EQUIVALENT UUNCERTAINTY IN ATMOSPHERIC BI-214 4PI CORRECTIONTO ONE DEICMAL PLACE IN PPM EQUIVALENT UAVERAGED URANIUM-TO-THORIUM RATIO TO ONE DECIMALPLACE IN PPM EQUIVALENT U PER PPM EQUIVALENTTHURANIUM-TO-THORIUM RATIO STANDARD DEVIATION FROMTHE MEAN TO ONE DECIMAL PLACE AND ALGEBRAICALLYSIGNEDAVERAGED URANIUM-TO-POTASSIUM RATIO TO ONE DECIMALPLACE IN PPM EQUIVALENT U PER PERCENT KTHORIUM-TO-POTASSIUM RATIO STANDARD DEVIATION FROMTHE MEAN TO ONE DECIMAL PLACE AND ALGEBRAICALLYSIGNEDAVERAGED THORIUM-TO-POTASSIUM RATIO TO ONE DECIMALPLACE IN PPM EQUIVALENT TH PER PERCENT KTHORIUM-TO-POTASSIUM RATIO STANDARD DEVIATION FROM THEMEAN TO ONE DECIMAL PLACE AND ALGEBRAICALLY SIGNEDThe remaining 440 characters in this block are blanks.Block 2 - Statistical Analysis Identification DataThe second block contains the identifier information for the datacontained in subsequent blocks according to the format specification inthe first part of Block 1. The final 6078 characters on this blockare blanks.Block 3 - Statistical Analysis DataThe third and subsequent blocks contain statistical analysis data inthe format specified by the second part of the Block 1. Fifty logicalrecords are allowed per block. The method for determining uncertaintyvalues shown, as of August 1979, remains undefined. These values arefilled with 9's under format control.F6.1F5.1F6.1F5.1******A24ITEM1234567811141616F8.4F8.4F6.1F7.1A814F6.1F4.1F5.1F6.1F4.1F5.1F6.1F4.1F5.1910111213141516171819A25MAGNETIC DATA TAPEREFERENCE: Paragraphs 4.7.8 and 6.1.6, BFEC 1200-C ITEMThe Magentic Data Tape is an unlabeled, nine track, 800 BPI, NRZI. Alldata are recorded as EBCDIC characters. Each tape contains data for nomore than one quadrangle and are divided into 8000-character blocks asdescribed below.Block 1 - Tape Format DescriptionThe first block contains 3384 characters of format information inexactly the following format:04 0978 (DATA TAPE TYPE AND FORMAT SPECIFICATION DATE CODES)678FORMATF8.4F6.1F5.1A8F7.1910111213F7.1F7.1F7.1DESCRIPTIONLONGITUDE TO FOUR DECIMAL PLACES IN DEGREESTERRAIN CLEARANCE TO ONE DECIMAL PLACE IN METERSOUTSIDE AIR PRESSURE TO ONE DECIMAL PLACE INMMHGSURFACE GEOLOGIC MAP UNIT CODETOTAL MAGNETIC FIELD INTENSITY TO ONE DECIMALPLACE IN GAMMASRESIDUAL (IGRF REMOVED) MAGNETIC FIELD INTENSITYTO ONE DECIMAL PLACE IN GAMMASDIURNAL MAGNETIC INTENSITY VARIATION TO ONEDECIMAL PLACE IN GAMMASMAGNETIC DEPTH-TO-BASEMENT TO ONE DECIMAL PLACE INMETERS (IF REQUIRED)MAGNETIC DATA TAPE The remaining 4616 characters in this block are blanks.FORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK)Block 2 - Magnetic Tape Identification DataITEM123456789FORMATA40A201413141613F8.4F8.410-14 (SAME)***** *495-499 (SAME)DESCRIPTIONQUADRANGLE NAME AS PROJECT IDENTIFICATIONNAME OF SUBCONTRACTORAPPROXIMATE DATE OF SURVEY (MONTH., YEARNUMBER OF FLIGHT LINES ON THIS TAPEFIRST FLIGHT LINE ON THIS TAPEFIRST RECORD NUMBER OF FIRST FLIGHT LINEJULIAN DATE (DAY OF YEAR) FIRST FLIGHT-LINE DATAWAS COLLECTEDLATITUDE OF GROUND BASE STATION TO FOUR DECIMALPLACES IN DEGREES FOR FIRST FLIGHT LINELONGITUDE OF GROUND BASE STATION TO FOUR DECIMALPLACES IN DEGREES FOR FIRST FLIGHT LINEREPEAT OF ITEMS 5-9 FOR SECOND FLIGHT LINE ON THISTAPE***REPEAT OF ITEMS 5-9 FOR 99th FLIGHT LINE ON THISTAPEThis block contains information about the data in subsequent blocksorganized according to the format specification in the first half ofBlock 1.Block 3 - Magnetic DataThis block and subsequent block contains magnetic data for the quad-rangle organized according to the format specifications in the secondhalf of Block 1. There will be 100 logical records per physical block.FORMAT FOR MAGNETIC DATA RECORD (THIRD THRU LAST BLOCK)ITEM FORMAT DESCRIPTION1 I1 AERIAL SYSTEM IDENTIFICATION CODE2 14 FLIGHT LINE NUMBER3 16 RECORD IDENTIFICATION NUMBER4 16 GMT TIME OF DAY (HHMMSS)5 F8.4 LATITUDE TO FOUR DECIMAL PLACES IN DEGREESA26STATISTIC ANALYSIS SUMMARY TAPEREFERENCE: Paragraphs 4.7.9, BFEC 1200-CThe statistical analysis summary tape is an unlabeled, nine track,800 BPI, NRZI. All data is recorded as EBCDIC characters. The blocklength is 700 characters long. Each tape contains one file of data forno more than one quadrangle.Block 1 - Format Description DataThe first physical block on this tape contains a format descriptionfor data on subsequent blocks. The first 4320 characters on thisblock contains 60 lines of 72 characters exactly as written below:05 0978 (DATA TAPE TYPE AND FORMAT SPECIFICATION DATE CODE)STATISTICAL ANALYSIS SUMMARY TAPE (OR FILE)FORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK)ITEM1234FORMATBLOCK)ITEM123456789101112131415FORMAT DESCRIPTIONA40 QUADRANGLE NAME AS PROJECT IDENTIFICATIONA20 NAME OF SUBCONTRACTOR14 APPROXIMATE DATE OF SURVEY (MONTH, YEAR)16 NUMBER OF GEOLOGIC MAP UNITS USED FOR THIS QUADRANGLEFOR STATISTICAL ANALYSIS SUMMARY DATA RECORD (THIRD THRU LASTFORMAT DESCRIPTIONA8 SURFACE GEOLOGIC MAP UNIT IDENTIFYING CODE16 TOTAL RECORDS FOR GEOLOGIC MAP UNIT16 NUMBER OF POTASSIUM RECORDS COMPUTED FOR GEOLOGICUNITF6.1 POTASSIUM CONCENTRATION MEAN TO ONE DECIMAL PLACEIN PERCENT KF6.1 POTASSIUM CONCENTRATION STANDARD DEVIATION TO ONEDECIMAL PLACE IN PERCENT KA3 POTASSIUM CONCENTRATION DISTRIBUTION CODE16 NUMBER OF URANIUM RECORDS COMPUTED FOR GEOLOGIC UNITF6.1 URANIUM CONCENTRATION MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT UF6.1 URANIUM CONCENTRATION STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT UA3 URANIUM CONCENTRATION DISTRIBUTION CODE16 NUMBER OF THORIUM RECORDS COMPUTED FOR GEOLOGIC UNITF6.1 THORIUM CONCENTRATION MEAN TO ONE DECIMAL PLACE INPPM EQUIVALENT THF6.1 THORIUM CONCENTRATION STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT THA3 THORIUM CONCENTRATION DISTRIBUTION CODE16 NUMBER OF URANIUM-TO-THORIUM RATIO RECORDS COMPUTEDFOR GEOLOGIC UNIT1617181920212223242526F6.1F6.1A316F6.1F6.1A316F6.1F6.1A3URANIUM-TO-THORIUM RATIO MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT U PER PPM EQUIVALENT U PER PPMEQUIVALENT THURANIUM-TO-THORIUM RATIO STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT U PER PPM EQUIVA-LENT THURANIUM-TO-THORIUM RATIO DISTRIBUTION CODENUMBER OF URANIUM-TO-POTASSIUM RATIO RECORDSCOMPUTED FOR GEOLOGIC UNITURANIUM -TO-POTASSIUM RATIO MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT U PER PERCENT KURANIUM-TO-POTASSIUM RATIO STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT U PER PERCENTURANIUM-TO-POTASSIUM RATIO DISTRIBUTIONNUMBER OF THORIUM-TO-POTASSIUM RATIO RECORDSCOMPUTED FOR GEOLOGIC UNITTHORIUM-TO-POTASSIUM RATIO MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT TH PER PERCENT KTHORIUM-TO-POTASSIUM RATIO STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT TH PER PERCENT KTHORIUM-TO-POTASSIUM RATIO DISTRIBUTION CODEThe remaining 2680 characters on this block shall be blanks.Block 2 - Statistical Analysis Identification DataThe second block contains the identifier information for the data con-tained in subsequent blocks according to the format specification in thefirst part of Block 1. The final 6930 characters on this block areblanks.Block 3 - Statistical Analysis Summary DataThe third and subsequent blocks contain statistical analysis data in theformat specified by the second part of the Block 1. Fifty logicalrecords are allowed per block.A27BIBLIOGRAPHYAdams, J. A. S., and Gasparini, P., 1970, Gamma-Ray Spectrometry ofRocks; Elsevier Publishing Co.Burson, Z. G., 1974, Airborne Surveys of Terrestrial Gamma Radiationin Environmental Research; IEEE Trans. Nucl. Sci., NS-21, No. 1, p.558-571.Currie, L. A., 1968, Limits for Qualitative Detection and QuantitativeDetermination; Analytical Chemistry, Vol. 40, No. 3, p. 586-593.Grasty, R. L., Uranium Measurement by Airborne Gamma-Ray Spectrometry;Geophysics, Vol. 40, No. 3, June 1975, p. 503-519.Gregory, A. F., and Horwood, J. L., 1963, A Spectrometric Study ofthe Attenuation in Air of Gamma Rays from Mineral Resources; U.S.Atomic Energy Commission Report CEX-60-3, Washington, D.C.McSharry, P. J. and Emerson, D. W., The Collection and Processingof Gamma Ray Spectrometer Data; 2nd International Conference onGeophysics of the Earth and Oceans, Sydney, Australia, January1973.APPENDIX B - Flight SummaryM-iT' Li LiiLj t -i____ LUAPPENDIX BDAILY PRODUCTION SUMMARYJANUARY, FEBRUARY, 1981QUEEN AIR N9AGJan. 12-1314-1516-17181920212223242526-28293031Feb. 12-3456-891011-1213141516-181920212223242526Aircraft MobilizationRadar Compensation, Magnetometer CalibrationWeather - Nil production988 Line Miles - Valdosta, Jacksonville940 Line Miles - Valdosta, Jacksonville716 Line Miles - Valdosta, Gainesville, Daytona BeachWeather - Nil production818 Line Miles - Valdosta, Gainesville, Daytona Beach749 Line Miles - Valdosta, Gainesville, Daytona Beach,Jacksonville721 Line Miles - Daytona Beach, Orlando, Tarpon Springs652 Line Miles - Gainesville, Daytona Beach, Orlando,Tarpon SpringsBase Mobilization994 Line Miles - Tarpon Springs,923 Line Miles - West Palm Beach,867 Line Miles - West Palm Beach,858 Line Miles - West Palm Beach,Weather - Nil production766 Line Miles - West Palm Beach,Fort PierceMagnetometer repairWeather - Nil production771 Line Miles - Tampa, West PalmMiami362 Line Miles - Tampa, West PalmMiami, Key WestTampa, Fort PierceTampa, Fort PierceTampa, Fort PierceTampa, MiamiOrlando, Miami,Jan. 10-111213-1920-222324252627-28293031Feb. 1-23-56-78-1213Base MobilizationWeather - Nil productionMagnetometer replaced and calibratedWeather - Nil production365 Line Miles - Brunswick, Waycross568 Line Miles - Brunswick, WaycrossEquipment Check452 Line Miles - Brunswick, WaycrossWeather - Nil production501 Line Miles - Brunswick, Waycross468 Line Miles - Brunswick, Waycross310 Line Miles - Brunswick, WaycrossWeather - Nil productionBase Mobilization and MaintenanceWeather - Nil productionEquipment repairs and testing225 Line Miles - ApalachicolaTotal for the above period = 2889.0 milesTotal miles for the included quadrangles:WaycrossBrunswickApal achicolaBeach, Fort Pierce,Beach, Fort Pierce,1897.0767.0225.0Base Mobilization480 Line Miles - AndalusiaWeather - Nil production719 Line Miles - DothanWeather - Nil production720 Line Miles - Tallahassee845 Line Miles - Andalusia1075 Line Miles - Andalusia, DothanWeather - Nil production541 Line Miles - Dothan, Tallahassee792 Line Miles - Tallahassee665 Line Miles - Pensacola, Andalusia682 Line Miles - Pensacola, Andalusia, DothanTotal for the above period = 17,644.0 milesTotal miles for the included quadrangles:ValdostaJacksonvilleGainesvilleDaytona BeachTarpon SpringsOrlandoTampaFort Pierce1907.0566.01251.0840.0737.01279.0624.01590.0West Palm BeachMiamiKey WestDothanPensacolaAndalusiaTallahasseeB1wb1709.0508.0114.01897.0914.01897.01811.0AERO COMMANDER N1213BAPPENDIX C - Flight Path and Geologic MapIWAYCROSS"4 10 - 81010 0200 _.1 .9_ 810 "- - '1_____ - - 10 -81________ 9-- BI - ______ _B1B84 oo2 83 0 8 1 0 8 11 0 8 8 10 1 - 1 2 0 0 0 1 5 5 0 0p1p s780 0 780 00 8 2 -------- 801-- T8 801 -88 7s800--- 700 700 7007 0 ~ ,0 2 807070_000-70'8 77 B -0 77se00-7 7o 77 2000 77077090mn80 07708--GA_ _ -_- 80 0 60.0 780707_SCALE 1.00,000-C' 110017B0110078FLIGHT-PTH]RECOVTpmup75 1 077 770.- -,770.5877701--7 7021770 - ---- r- 770 -12 8 17 7 02_______e_ _-60_ 7-_ 60--- -- 7 77 2171 817 MIS-ISSII2 FLORIDA-P J31 3 e- -750 75 5 5-07500 AHA-y uj749 * 740 30071 70- - wpm yegg 7 80 74 - 0 -vAVT To m h7 5-131 31 - 0 - sLeTms3 au se 7 3 -I-3Ton +Qop72 2 2 a 72- - - 7_21 s m- 4 6" 720 - 2 t S720 - "gyp 720- ]e 20 720 - 0 7SCALE 80100 1.500.EAM00 L0 1N N17-IHT PAH0EC V......,I " F 0080, "w COMP6lD 108 N'^189 177 0505505 . S'DPARMENnOF EN" W . +m m. u"x ) )1 X11lnppI97 .713 10 7s NH __70 NO71 31 M1191 1772mm Tmh -o'NT15 NHMSSS IPI L RIAhR J- "' Jf_ 'TGO ----- S -- Ggg T 7 F01 Ae 9~-7- -E82 0032 00CTpmuTpmu771TpmuWT- 31 3095000 746820 1ERYECCaTNGBRUNSWICK82 0032 00 Qpm801 , ()atD~m a1mG~pps TpmlpGhanmlalppra( _ 1 al..70 6790 - 760 7 790 7 0 79760 7ranmm t Ol0atlmmQtpoPmpGhmTpmutT~mu N OW Gp1 am am a h760 7. 60 76 74 3 8 5OEmaltl alprapr-h1 m GcmGall\ patGpaGtp"I 0nm anmTemamnm731___ 7 31 - '731 7 0Tpcd G, anmh31001"i . .hrr n,82 paahm ohmGhm Q Qsb Ohmhm 251qhmQtsbOhl0jBo0ooal 00INDEX TOADJOINING SHEETS< 0VA1N0NGEORGIA-LOSTA 1) TETSON MESAbmmsaN ron Rxckrele, M. y" 1R2052FLIGHT PATH RECOVERYMISSISSIPPI/ FLORIDA PROJECTU. S. DEPARTMENT OF ENERGYO 00WAWA(G EGG GEOMETRICSSCALE 1 500,000l__________________ ____ ____________ __________ -i uoI1w b81 00--JO1 301- s3 -D LIN N- s!HT LINE SPACING 6.0 MILE(S)3T ALTITUDE 400 FEET AMTIN AND COMPILED 1990SURVEY ANDCOMPILATION BY'1C3wbWAYCROSS QUADRANGLEGEOLOGIC MAP EXPLANATION(Martel Laboratories, 1981)bFQtsb71{QtpramQtpraQTpps PLEISTOCENE-PLIOCENE SANDS AND GRAVELS,UNDIFFERENTIATED: INCLUDES THE SUNDERLAND, COHARIE ANDBRANDYWINE FORMATIONSTpcd CHARLTON FORMATION AND DUPLIN MARL,UNDIFFERENTIATEDTpmu PLIOCENE AND MIOCENE SEDIMENTARY ROCKS,UNDIFFERENTIATEDSEDIMENTARY ROCKSALLUVIUM: ALLUVIAL DEPOSITS OF PRESENT STREAMSEOLIAN SAND DEPOSITSHOLOCENE COASTAL MARSH DEPOSITSHOLOCENE COASTAL BARRIER ISLAND DEPOSITSSILVER BLUFF TERRACE DEPOSITSPRINCESS ANNE TERRACE MARSH DEPOSITS: ALLUVIALDEPOSITS OF THE LATE PEORIAN INTERGLACIAL PERIODPRINCESS ANNE TERRACE BARRIER ISLAND DEPOSITS:ALLUVIAL DEPOSITS OF THE LATE PEORIAN INTERGLACIAL PERIODPAMLICO TERRACE MARSH DEPOSITS: ALLUVIAL DEPOSITS OFTHE PEORIAN INTERGLACIAL PERIODPAMLICO TERRACE BARRIER ISLAND DEPOSITS: ALLUVIALDEPOSITS OF THE PEORIAN INTERGLACIAL PERIODTALBOT TERRACE MARSH DEPOSITS: ALLUVIAL DEPOSITS OF THELATE SANGAMON INTERGLACIAL PERIODTALBOT TERRACE BARRIER ISLAND DEPOSITS: ALLUVIALDEPOSITS OF THE LATE SANGAMON INTERGLACIAL PERIODPENHOLOWAY TERRACE MARSH DEPOSITS: ALLUVIAL DEPOSITSOF THE MID-SANGAMON INTERGLACIAL PERIODPENHOLOWAY TERRACE BARRIER ISLAND DEPOSITS:ALLUVIAL DEPOSITS OF THE MID-SANGAMON INTERGLACIAL PERIODWICOMICO TERRACE MARSH DEPOSITS: ALLUVIAL DEPOSITSOF THE EARLY SANGAMON INTERGLACIAL PERIODWICOMICO TERRACE BARRIER ISLAND DEPOSITS: ALLUVIALDEPOSITS OF THE EARLY SANGAMON INTERGLACIAL PERIODIIOrOmmZm-0C)mzmIO-)mZOzmZ->CDmzD1'QipaIQttmLQtti6tpemtQtpeiQtwmQtwiU0zUC4wbBRUNSWICK QUADRANGLEGEOLOGIC MAP EXPLANATION(Martel Laboratories, 1981)ALLUVIUM:HOLOCENE ALLUVIAL DEPOSITSLOESS: MASSIVE BED OF BROWN CLAYEY AND SANDY SILTPENHOLOWAY TERRACE MARSH DEPOSITS: ALLUVIAL DEPOSITSOF THE MID-SANGAMON INTERGLACIAL PERIODPENHOLOWAY TERRACE BARRIER ISLAND DEPOSITS:ALLUVIAL DEPOSITS OF THE MID-SANGAMON INTERGLACIAL PERIODWICOMICO TERRACE MARSH DEPOSITS: ALLUVIAL DEPOSITSOF THE EARLY SANGAMON INTERGLACIAL PERIODWICOMICO TERRACE BARRIER ISLAND DEPOSITS: ALLUVIALDEPOSITS OF THE EARLY SANGAMON INTERGLACIAL PERIODPLEISTOCENE-PLIOCENE SANDS AND GRAVELS,UNDIFFERENTIATED: INCLUDES THE SUNDERLAND, COHARIE ANDBRANDYWINE FORMATIONSQalQtpem6wmQtw6lppsTpmul[Tmh[mmF TosTeo7HAWTHORN FORMATION: MARINE SANDS, CLAYS. MARLS AND SANDYLIMESTONES ALL OF WHICH ARE PHOSPHORITICMICCOSUKEE FORMATION: YELLOWISH RED, CROSS-BEDDED, THINLYLAMINATED, SILTY, CLAYEY QUARTZ SANDSSUWANNEE LIMESTONE: GRANULAR THIN-BEDDED, SOFT, SHALLOWMARINE, HIGHLY FOSSILIFEROUS LIMESTONE. WITH PORTIONS HIGHLYDOLOMITIZEDOCALA LIMESTONEIII0C)mzmmC)mzmzvC)mzm0zm0r-0C)mzmm0C)mmIr_OC)mzmCcmzzm-4Cmz-40NJ0zWU0PLIOCENE AND MIOCENE SEDIMENTARY ROCKS,UNDIFFERENTIATEDAPPENDIX D - ProfilesD1wb. 0- 7 -.- 70-2B 7]0000 - 700 7-I 700 - 7gB ]P.1 I I I I I I I Ii IIF-- I-UI-- -- z t iL JTaI d1 IA1l~ 1 1 ilTl I II I .LFTL/KMIN .D0E 0MAX 65.94MEAN 1.893STD 0EV 8.003BI /KMI NMAXMEANSTD 0EV000021.82.63772.843Ii1 1Jppz-UO - ~ I~ A .rCDNrmIco.m gLag Ail-ElF _____________I-F-al:m:0m:c---a- ----s-----------___---.----- -------- --------------------------\- ' - - --- - --[3JF-LoILt ICBI/TLMIN .0000MAX 2.018MEAN .356.STD DEV .3171TOTAL COUNTSCTS/2SECMIN 71.53MAX 1463MEAN 536.9STD DEV 281.1POTASSIUM 40PERCENTMIN .0794MAX .2MEAN .1241STD DEV .0243BISMUTH 214EO. PPMMIN .644-MAX 3.321MEAN 1.421STD DEV .5087THALLIUM 208EQ. PPMMIN .6689MAX 8.838MEAN 2.831STD 0EV 1.79481 AIR CORREQ. PPMMIN .2613MAX 1.882MEAN .8679STD 0EV .3763RESID MAGGAMMASMIN -938.4MAX -383.1MEAN -663.8STD DEV 171.3RADAR ALTMTAFEETMIN 303.2MAX 522.8MEAN 386.8STO 0EV 23.66LINE 700-NzzmNw 0Wcrr 0CE FI~U-3I,a'6IIIIF mm 1IH:H Fx-- - - -- - --- - '- '-~~-'- ----- - - - - - ---- _ _ __-- - ---- ---- - -..II I Ii mL-----------------IL.11.1 I 1 1.1 1, 1 ti I--l-IL I II_mII4rmULLQ_---I - - - Nf-\ - Lm--\.' \_/ -\f --- - -,./ - - w -\,/ \,-- \T W - C5- - V - v Q v v'o ."mA 00 o n"ne-7I ne -N 70 1 - n a , _ e- 710 110D2wb710 -- ----FI-M- _______ _1__ __. ______ _v~ H~1~_________IL. -El---L 1 9E9 E3 ElEl m,4 -_E3 -BEl E3E_ _g mjaa---IVA.. f--- - s- - -- - -- --- - -- - - --- --------------------------------------BI/KMINMAXMEANSTD DEVBI/TLMINMAXMEANSTD 0EV.000018.58.79033.042.00001.612. 4607.3248TOTAL COUNTSCTS/SECMIN 206.5MAX 1110MEAN 573.0STD DEV 200.4POTASSIUM 40PERCENTMIN .0834MAX .2299MEAN .1252STOD EV .0245BISMUTH 214"ED. PPMMIN .6467MAX 3.192MEAN 1.385STO DEV .4656J0F-O-Lzr,^-JLoNB AIR CORAED. PPMMIN .3988MAX 1.410MEAN .8857STD DEV .2354RESIDE MASGAMMASMIN -888.4MAX 133.0MEAN -549.7STD DEV 298.1RADAA ALTMTRFEETMIN 310.7MAX 475.2MEAN 391.1STD EV 25.35LINE 710zcozaU)Lr)THALLI UtEQ. FMI NMAXMEANSTD 0EVTL/KMIN .0000MAX 51.19MEAN 2.100STD DEV 7.88M 208PPM.67697.1822.5521.363g:u~ ra: oH HrH-Ja:Za:Q:OQ:a:Le- -----------------------------------------------------------------------------------------------------------------------------------------------------es e--.I'sM----Kr-------- ---111t(-711---"--T-22j - 7 21 72 720- ---- 720-d 720 720 7r - -- r11iC , I1UIn 1 I- SMI~ I ~ _______________________________________________________________.. i III I L iJH-HI.CFCFlf6Cfo6:JJ:Z9 Y * N M M 0I N NJNNc NmDDC_ _ _ -NC D CDC DCDC DCniC DC DC DC DCII A A A nF-U).mLa~1t C :.;: :=1=-i CMCINMAXMEANSTD EVBI/TLMINMAXMEANSTD DEVTOTALC1TODEVN00miJ uL------.000072. 134.84+712.07. 000021.541.5994l.015.00001 .740*45112627OUNTSSEC59.031348596.9202.2POTASSIUM 40PERCENTMIN .0802MAX .7373MEAN .1577STD DEV .0917BISMUTH 214EQ. PPMMIN .6694MAX 2.827MEAN 1.351STD EV 3929THALLIUM 208EQ. PPMMIN 68746MAX 9.300MEAN 2.934STD DEV 1 .469BI AIR CORREQ. PPMMIN .3082MAX 1.483MEAN .7278STD EV .2818RESIDE MAGGAMMASMIN -851.0MAX 583.1MEAN -535.7SD DEV 389.8RADAR ALTMTRFEETMIN 326.5MAX 451.0MEAN 385.8STD EV 19.49L INF 720JF-LY~~"_zU)zwGz lcr(I)0D3wb- 2 -771 __TL/KMINMAXMEANSTD DEVBI/K00a:NEDuJCE0a-LU------------- -------------- --....- ------ ---------------------------------------------------1111111.IT-LI A. . I II III 111IlL 1, 1i! l k riii- ---; ,m -.- -- -I mm now Ni a iul%1----------------------------------------------------- - -- -- - - - - - - --- -------------- - Her -vvu -d f-11 ga l I.1ii1FrrtEffI.-mMWw f=afir---------Irv v ' ,--- - v''ZN 73 - - e 731 s a31 r s e3 e 731 e 7CL^rmi~ 11 '4 III A IPiT Kw w~ ~ANVV~f~r^\TL/KMINMAXD10EV____STD DEVBI/KNTDDEVBI/TLP> T (VWJ PEVL . I -- 1-' " Y 114 III - - - 11 1 1 nl i ir0 N ~.14. CDA4 -I- !0~UH-Lm~.000069.386.64513.65.000021.081.9584.270.00001.610. 4096.2 445zCowc00CC)F-HLmFJF-rnoar t.mfDmu Oalpmu CTpPaCal Ctp mCTPP,e 73t eee T ee 73l 40e oDi i 1 e 1m fa oDiCt-TpmuP ^ _D4wbTOTAL COUNTSCTS/ SECMIN 111.2MAX 1324MEAN 658.8STOD EV 232.9POTASSIUM 40PERCENTMIN .MAX .3124MEAN .1575STD DEV .0538BISMUTH 214EQ. PPMMIN .6591MAX 2.961MEAN 1.441STD EV .4332THALLIUM 208E0. PPMMIN .6948MAX 9.050MEAN 3.539STD 0EV 1.789BI AIA COREQ. PPMMIN .3633MAX 1.338MEAN .7222STO 0EV .1902RESIDE MAOGAMMASMIN -922.4MAX -3.836MEAN -644.0STO DEV 188.2RADAR ALTMTRFEETMIN 319.6MAX 482.8MEAN 387.2STD DEV 23.06LINE 730A i . ,C:LIaCf'uucFc0I'hUs arnsBmLo(Dinmww Ftmmc0-U:Eru-H-JICa.Lm- ~ ~~~~ -.- ' ---n - -~ - -- - -- - - ----- -- -- --_ _ - --------- --- -- --- - - x -- - - - - - - - - -i '-,, - C)u-- /- ---N I, 1-j- EK I,Cv V-,-.'- vIimm mm Ipm pm.Dtpp m o001,m l -___ .---- ope-- I I IIid j -!i 1 - ~~~iT I 17IFFh u I nJ I i A1111-- --iI77"T1 i7DL IIFH F h1[ ]i-iL IF -lizil H ITL/KMINMAX-MEANSTD 0EVcol HBI/KMI NMAXMEANSTD DEVBI/TLMINMAX.. I~~ JRMEANAkA~~.r~.PPN /~V~..A ~ FMf~~A I -STD 0EV7 _ ________________________________________NN ~ti-91)mW v V..000080.506.65114.50O.000020.651.-9834.37400001 .30*405.200TOTAL COUNTSCTS/SECMIN 243.0MAX 1340MEAN 670.0STD DEV 189.1POTASSIUM 40PERCENTMIN .0797MAX .2810MEAN .1321STN DEV .0322BISMUTH 214EQ. PPMMIN .6841MAX 2.931MEAN 1 . 406STD DEV .3884THALLIUM 208EQ. PPMMIN .6892MAX 9.948MEAN 3.560STD DEV 1.608BI AIR COREQ. PPMMIN .3390MAX .9960MEAN .6985STD DEV .1374RESID MAGGAMMASMIN -883.0MAX 249.4MEAN -554.3STD DEV 282.6RADAR ALTMTRFEETMIN 323.1MAX 453.3MEAN 387.5STD 0EV 22.10LINE 740[r I9 li i I II1111D _vri ~fUI~1011I I I I 1 If*i BrJF ii iiC g i i N I N i I H! 1 1H M 1 lHhwii i iR fD5 wb_______________ ~vff~AJA~v~I\zCOwCT)CU)mI-rIF-zLQF-F-Lr6UUaF-caLF-vIIrWQtsnm-ANAA4--ai:L .L7QDwjac0m.JCCEDLm~- - ~------------- -- - - - - - - - - _ _ __ ______________________i- -----$ -------g -------- ----------- - - ------- - - -- VIIR #! i m " Rig Mkiii A Mi ii i i m 0 i i Ni i i iii A i. i i M i HwHi 1 0 H HA i Itmi r ui m e III 1 1111 11 1 0 in i 1 ;1;;;;) 1 II 11 I p III Mil I I I W I 141 11I I ® M II 5 11 1 1 1 111 fl I iI 1 1.1 1 -49 LlJLLIL-L _1 1 u a 1111 11 u -I"" { N 4F 1 1 t tIIIicJ"l I ;"A -- Ia-A- -- AA_Lr r- ----- - -- - - =5_ ____ 5- _-- 5- f ' --- -' 5 --. __55_S_ -.-. - -- - - -'Si - '-,IIIAll .lftf-- 'd! 1';lf i I iM rI1 -11 1I lIJIliIL_11I1L!IIll f JI MII ',e. i_I l'tM1VI,.ill I I II j I__,,r I I I_rI V-1-v-." , On , A ./%-_ r" I_ _tffl v ~ Z v .r V v - -" v V -,vu W -%-\.I " vv Ve 75 5 7-0-7 750 0 750-IV -30000 750'3 --m1D6whPm IPmu rompDmCTPDTI BCPI GaljQTDD.BBeNO m 36tng750 37800 750 3780e 750 3720 7 378 0 ,mP 750 50f9GPITpmu pmuTpmu" \\\\ (\\ \ GPIK LmiE~ zz taiti~ ______I L U, 1J ________________________ __~~~- -J--J)~~p~A~fv\~A ~ ~.y~~x~~ ~Atm- --- -- - -mDm0 N60m0 mDm N1 11 p\-,"'I -VTL/KMINMAXMEANSTOD EVBI/KMAXMEANSTD DEVBI/TLMINMAXMEANSTD DEV.000066. 467.33914.47.000022.632.2434.662.00001.227.3959. 1930TOTAL COUNTSCTS/SECMIN 246.5MAX 1219MEAN 696.8STD DEV 192.3POTASSIUM 40PERCENTMIN .0807MAX .5683MEAN .1583STD DEV .0738BISMUTH 214ED. PPM-zCJrC- criif1MIN .6651MAX 2.813MEAN 1.401STD EV 078THALLIUM 208ED. PPMMIN .8024MAX 8.896MEAN 3.791STD EV 1.552BI AIR CORREQ. PPMMIN .3420MAX 1.009MEAN .6755STD DEV .1513RESIDE MAGGAMMASMIN -958.9MAX 53.64MEAN -579.2STD 0EV 257.3RADAR ALTMTRFEETMIN 329.1MAX 500.9MEAN 393.5STD 0EV 23.92LINT 750H-11r-0101H& m00CD C05 1mm0UH Fco Z~6.3Q:0J0Lm------------ ----------------------------------------------------------------------- K----- -- -- -- ----------------------------------------------------------------------------------------------------------------------------- ---------------------------------------------------.I U U'-- tttt_n0\-'n-I i AM t i i-- - -Mm in - 1 M--I -- -fI -6m-- 10(i in-----F --- , rc 1v V v ..- v u-'I - -NWJLrmmn=pFrik N9rr-. _f01J0 - - --- -760- --- - 760 2200 760-' ii .1 lzI~~zz~s ii I I iz1 1 AlIIIiniz zzib Mi fh-1 11I _Ii Ui l I1 1 1i I' 1 4'I I f 11 ri fi I~I ~- - I f --?Irr i-®--U-_-- . W - -- 1i - ____®m______ - n _I ii I II I IE L JL i.I LL IIJ II.. - E3 11 I -Ii IiTIA LI - 'A _ ________________________________________ I- I AVV AAAI~r~AA~/\~V> A(~&~ PI ,o'I,,'''lA 7, ' 8J , ', eA 11 ,11 111/1-:TL/KMI NMIAXMEANSTD DEVBI/KMINMAXMEANSD DEVBI/TL-JLm-IL.J'I I P ' \ W fIIll I I R1 IC EV_ -_ __-_ \ e---- - - -- -- -- - - --- -- H __ _-_08)N_ - e.000072.076.43313.57.000019.852.1454.67400001.576. 4153.2126TOTAL COUNTSCTS/SECMIN 479.6MAX 1505MEAN 948.4STD DEV 185.2POTASSIUM 40PERCENTMIN .0964MAX .3499MEAN .1605STOD EV .0431BISMUTH 214E. PPMMIN .9007MAX 3.206MEAN 1.813STD DEV .4362THALLIUM 208EQ. PPMMIN .8414MAX 9.852MEAN 4.317STC 0EV 1.655BI AIR CUEQ. PPMINMAXMEANSTD DEVRESID MAGGAMMASRR1 .4062.3562.010.1919MIN -1129MAX 42.90MEAN -713.8STD 0EV 262.0RADA ALTMTRFEETMIN 331.0MAX 445.4MEAN 387.9STD DEV 18.74LINE 760Fit T 4-.I I i 11 1 1IN I itD7wbMINMAXMEI128FrzFILC0LacN,JcrILILC0LwLL-AS-ACwCD yC-)0ILOLvLIILILNof " 1 n N~et - r~m *--Tp-C10PL mmm IPmuNCal-760" zLSec 7 Lee 760 a QTPP- 7Cai(P IPmumICfPPt TPmu Tpmu rom.Cai l \ ^ ^ OaliA,' lil f4lfliII R IFni11 , r "' I li 94 1 I! t1 A 11 I xi-Iiiii& \/ - "- -~-s. - '~ v'vrf. v o.--.--a o sfv- -,.- 760 ---- ----I I ! II i I11 Im.Fcv - - v V -ur,/ - - - vV .--' _ l70Bu770 770-- -V - 770-romuzU)WcZr-CoC?CCr - iHI .l AI II ti liV i I 1 IiL1~ 1i'H'E~iLL_ _I I I J I 111 hI1 1~~~TL/KMINMAXMEANSTD 0EVBI/KSTD DEV- -1-/TL.000075.844.74512.12.000020.931:.4E73.896. 0000I.974. 4673.2523TOTAL COUNTSCTS/SECMIN 539.8MAX 1618MEAN 932.9STD EV 196.5POTASSIUM 40PERCENTMIN .1014MAX .3339MEAN .1670SID 0EV .0438BISMUTH 214EQ. PPMMIN .8923MAX 3.714MEAN 1.792STD EV .4553THALLIUM 208EQ. PPMMIN .9140MAX 11.16MEAN 3.985STD DEV 1.895BI AIR CORREQ. PPMMIN 1.756MAX 2.729MEAN 2.152STO DEV .2045RESIDE MAOGAMMASMIN -1279MAX -263.7MEAN -872.6STDIOEV 242.4RADAR ALTMTRFEETMIN 31.4MAX 462.0MEAN 391.7STD 0EV 21.07LINT 770770 - 7703 -a 770 770-iLmmII. IJH nvD8wbUiLi ~ I __ ffl11 [ Fl I ~1~~Y't I~iIi ~Lm~NIIorA-JQ 0I3- ---_F-cF-LF6aCrC aF-CaLIC\F-EClsam Lc ra6nFaF-LafuLiaraF-EF-aaacaL2I- ik ~ IMAX.4 4II4~~y4MEANj~f/~ VV~Y~ ~STD 0EV0:U0:_0:moJLmi i i i 9 H A t i i fl i mi " i ff i m i i m i H f i m i f litif i ji i mH vi m iIl 01 lil d 5 ii i d4l a$L-- I----- -EfFLL- r11iIH I N d 1W I N 91111 Ilflf 1_"-rNmWWIJ't'~ 770-I I ,IL -- A --D9 wb- _ --- 1 780--- --- -T - "1p ------ - --- -_____ _N IIi--z0r)co00DCEIII .. I .alJUII II I IIIIII 'J II II Ut I II--BI/KMINMAXMEANSTD DEVBI/TLMINMAXMEANSID DEV.000066.9111.5316.83.000020. 183.3055.032.00001.259.3703.1887TOTAL COUNTSCTS/SECMIN 300.3MAX 1488MEAN 772.6STD DEV 222.5POTASSIUM 40PERCENTMIN .0877MAX .59MEAN .1921STD DEV .0975BISMUTH 214EQ. PPMMIN 7434MAX 3.011MEAN 1.527STD DEV .4055THALLIUM 208ED. PPMMIN G 9698MAX 9.907MEAN 4.308STD 0EV 1.833LI AIR CORED. PPMMIN .5323MAX 1.291MEAN .8288STO 0EV .1634RESID MAGGAMMASMIN -1449MAX -582.2MEAN -1028STD 0EV 178.7RADAR ALTMTRFEETrMIN 323.9MAX 471.8MEAN 393.5STO DEV 22.59LINE 7807 780 --la ees w esa e780 68~ 80 8~ 8~ 78078 7oo78e V Y r 1 11 II II IA ( }} II Ven0)Q: 1 PIP, ,H-JH,L7 .-2 ______________________________F__ _________ -------------------------------------------- 2-_-___-- - - -- - - -- - - ---___- - -- - - -- - - -H -H-FR74Ii I-TL/KMINMAXMEANSTD DEVLsm:CUm:mrSQ m-- ---rnmu--F amIm- - i, r -- v T NIT6t 1 7 7 9 0 e-I"Ai ~t HHE * 1 11 11 1 1111111 , i i a IIII I I 1 1 1 u u u l a-I r 1 1 ua-ni--ryv--If!- ii i Mi d 1 1 Ml111 %W VA1111 i tiN I 11l I tI III!I 11 I II I Im I a it a1 k AA liii I ~I ig I ITi1[ n t- _t $ I I I ii w II '' * I ' I Ii 11 ~ 1 1.1 1....JLIUI JJI ) i ____ UI ...L.........Hill I...1...I~IIlo .ll la IIII II II II III fTl j lIii I I JI II III IIp® I L.L...I L..IlJ......I III II mIII III I;~ ~E 4Ihik% _ _ _____________________________ilJf-LaLF"JH-mN=lmz0U)J mAA f0 ' ~ f''ifNm pF-a:HI WLKST NDEVILL IILILIIIBI/KMI NMAXMEANSTD 0EV.000074.5313.016.82*000022.673.9075.187ITLMIN .0000MAX 1.802______________ -MEAN .3786~'~~o~,-~ STD 0EV .1973I - -_______--------------- - ------------- X ---------------- - - - -- - - - -- m~-TOTAL COUNTSCTS/SECMIN 349.5MAX 1794MEAN 833.3STD EV 320.7POTASSIUM 40PERCENTMIN .0830MEAN .2476STOD EV .1457BISMUTH 214ED. PPMMIN .7087MAX 3.910MEAN 1.68sO DEV .6121THALLIUM 208EQ. PPMMIN .7526MAX 11.39MEAN 4.628STD DEV 2.321i of o1,BI AR CMINMAXMEANSTD 0EVRESID MAGiim- -itEfe1rGAMMASMIN -1286~--IMAX -519.8_N_-947.3 SSf0 0FV 165.0JVV-'V s-' N~-'\J\f -'.' N' ~ ~NJN-' .. , A~. - -~ ~--.--' ~ A t'NRADAR ALTMTRFEETMIN 311.6MAX 470.3MEAN 384.2STD DEV 25.64LINE 790__ " t- r * ir iii i T INIE I lt1'. [jM l)t tfW \II ~ ~ fJ~/~~V-l. u ..ld ll ll ii .-ai111111zU)F'N1wZ)C)0:FCCFCF-s_UUFCCUI-._QWic_"-ftL9L:pQ'O:Ud0a:rCU)IiiF'yI--JQ:a:-Q:OQ:-'n " II 11111 I. 1v11U1' I II II I I A 1 e Ill L4I / v "1 11A All I II III I 1 11 11 1 A I in II=ME HL I I {' i in HI 1 1 ' 1 ri U {ICORRPPM.37 101.143.7680.1695ii_--- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ~- - - - - -- - --- ---- -- --- - --- - -- - - -9 -J~V 49 .11, -,%/ -- Er ^ -- ' W- - --ID1 0IIwb790791 n 1111144411 -1 1 1H II1 1 1H 1tI --. IimL\X- - 1-1 - -- m- - \,- \0' - ur -\4'S ae -801 - - - - - - - - 801 5 801-8 N-180 -8 01 1510 !8 - 801m GalGol cWAmmOul rpm.-601 see 801 2 801 i6ree s e 801 6900 01tpmu N WAQalotpps mm r 1J 9___________e__ht~ I1~E3 F9K\ m ___________________ _____ ____________________s?_____Alk(DlI4i1 Lb_ __ __ _ __TL/KMI NMAXMEANSTD 0EVBI/KMI NMAXMEANSTOD EVBI/TLMINMAXMEAN~-'-~A~STO 0EVCCr0CEcE-Iraf-IF03zF--wHr=0v.000075.3613.7616.35.000024.804.8085.867.00001.116.3977.1322TOTAL COUNTSCTS/SECMIN 332.1MAX 1960MEAN 1209STD DEV 238.4POTASSIUM 40PERCENTMIN .1040MAX .7786MEAN .2478STD DEV .1276BISMUTH 214ED. PPMMIN .9645MAX 4.651MEN 2.251STNDEV .6391THALLIUM 208EQ. PPMMIN .8928MAX 10.34MEAN 5.633STD DEV 1.67381 AIR CORAREQ. PPMMIN 1.517MAX 2.886MEAN 2.323STOD EV .3031RESI 8MRGAMMASMIN -1043MAX -640.9MEAN -881.9STO DEV 97.14ADAR ALTMTRFEETMIN 311.2MAX 482.9MEAN 393.7STD DEV 26.70LINT 800ID11wbat 6 0 -_._. N m/D mCO8 -j-9----------__ _ _ _ _ _ ____---- -_-.----...- - - - -- -. -_--- --- ~ -te r - n -m-- - - - --- - - -L1~L L~4N~-J-JCL0-JCCCLia:-CU-H:H FM -V -v --iiimiiii6__ _ _ _--iL0I f-In vffvn"V' GV- - -- -- \;', - M - -V N7I.I Iiim=-810 a 810-N9ZNe_ 810--610-mnQai( 1leve B10zee 10 e ee -810ll~ 0 .see 7 **- f I- i _l0 F~i~I1U- - -i--i- -- -- -F T-.--i--_-_---_------_IA~ I IiJJ 1 11 l II-U -' -i HflTMFt1,IA1 dUUTL/KMINjf-__MAXSTD 0EVBI/KMINMAXMEANSTD DEVrHmsa L ma r n { ~r~ [Am _ .-r, ̂J ______ f___________________~ ,~- -. --~ ~~ _ ~ --..-ELm .L m~W-RikI_____-_BI/TLMINMEANj m I STD 0EVIrSISIv~ "1000067.0012.2E16.9500002.614.0395.773.00001 .376.3635. 1415TOTAL COUNTSCTS/SECMIN 293.7MAX 2201MEAN 1189STD DEV 252.0POTASSIUM 40PERCENTMIN .1111MAX .7952MEAN .2252STD DEV .1156BISMUTH 214,EQ. PPMMIN .9139MAX 4.637MEAN 2.092STD EV .5671THALLIUM 208ED. PPMMIN .8988MAX 12.91MEAN 5.651STOD EV 1.816BI AIAECORREQ. PPMMIN 1.633MAX 2.967MEAN 2.476STD 0EV .2343RESIDE MAGGAMMASMINMAXMEANSTD 0EV-950.2-705.8-846.158.30RADAREALTMTRFEETMIN 300.4MAX 485.7MEAN 389.0STD DEV 25.20LINE 810I-- 810-[WJH-L mKmD1 2wbzwoLU- 0ci>-Cf)CL:3-cfic~ChCh-C.fu.awWr=aa1039Y-F-JCEa:CE00:LmtA 1'rvVJ-L---/V \ = y - = = '- -I-, IIErr- rm-- lI -------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------IM 8__ __ _ _t h I li Iill j1h I III .1 a IlIA 1 I, 11 , I . 11 . I I[1-Le ii JrxCCLCrr1',I -tn- -.- y3-\A .r,I xf-T[ TfY1fIQTT-- i T -m IliIi I N I L IiD13bma3VIze S Izee oft m lzee i .,s,---m-- zae fin 021Zamm n_ at___ 1 T I______ ______________ _________IA1 Jt TL/KBI/KMEANETDDEVI m BI/TLI-m0u-IQSrGIU)0a_F-I RNN N NODC-J-Lma:MN .0000IMAX 1.028STD 0EV .2229TOTAL COUNTSCTS/SECMN 213.5M AX 1984MEAN 512.7NTD DEV 212.3POTASSIUM 40PERCENTMIN .0818MAX 1.548MEAN .2114STD DEV .2118BISMUTH 21EQ. PPMMTN .5952MAX 3.126MEN 1.200STO 0EV .3820THALLIUM 208EQ. PPMMN .9022MAX 9.685MEAN 2.852STD 0EV 1.46781 AIRCEQ.PMNHMAXMEANSTD 0EVRESID NAGGAMMASMN -MAX -MIEAN -STO DEVCORRPPM.039 1.7048.2984/ .1034995.4418.8785 .2150.3RADAR ALTMTRFEETMIN 293.9MAX 447.4MEAN 385.9STD DEV 23.57I LINEa.:'CK I m II i. i .1zCoW co0ODD0Uf)r.000054.045.35411 .06.008814.341.3783.232-R,-c0U.a:m:I... IL IiAP,arC Qts0I1TrrrFrrrriiiTjvCMEChrccc.120036110 19 r 18us 1e19amL/oD1 4wt- MIN 0000MAX 22.12______MEAN 5.498hI S~TD DEV 1.6f -BI/TLMIN .0000FMAX 1.594MEAN .4178NDST EV .2777-- _Z TOTAL COUNTSZ CTS/SECp- MIN 218.0UMAX 1368MEAN 530.2ST-- EV 250.6Lo7_ _ _ _ _POTASSIUM 40PERCENTMIN .0739" )MAX .6231MEAN .2240U) ______STD 0EV . 1398- BISMUTH 214EO. PPMI--MIN .6047______________________________MAX 3.201-- MEAN 1.248D _ -STD DEV .4281---- - - - - - -. THALLIUM 208EQ. PPMMIN .7578MAX 10.176H) -- - -________ MEA .9STDEV 1.881L BL AIR CORRa:N _____________________________________ MAX .6539MEAN .3519rISTD 0EV .1218U) __________________ -~_____________RESID MAGU) GAMMAS______________-__-__ MIN -1192Ir ~MAX -701.8D - - - - - - - - - - - - - - - - - - - -- ------------- -- -- --- ------ MEAN -88.1S- RADAR ALTMTRJnMIN 313.401 MAX 44.a:ASTD 0EV 19.81a:a:-LINE 1190zU)-A cwoJwCCrLLCE-ma:ta:50U-a:a:iBD15b- BI/- - -- - er - -L10 2:8a11 0270 ITL/KMAX 8f8MEAN .881STD DEV 1.86)m- -- - - - _(-- T I/K C/ 0Cr-- ___ _---_ MAX26 2-F -.- MEAN 7. 9Ct ---- _-_-~--_ST DEV 5.063LJ----------------- MIN 0000MAX .422H_ _ _ _ _ _ _ _ _ _ __NST DEV .2376- E -r- ----- ISUH23- --_-- CTS/SEC-- - -M IN .2 7 20C~j MAX 9.432L-;------ - MEAN 7 .7. 2-_STD DEV 200.500 _____ _BIR_ _RR--- -------- ------ MIN G .0798S--- - MAX ' 428 .-a- -- _-- - - -U7- -S-D E ADEV .10 7-r -Oh-}- -- ---- ------- ------- - E A E 1LT 2TPTASSLIUM p-- --M A NDE.0 8 2-L--ST 0EV .1083crl__________________________ _-__-__-_____8AIR CORAE. PPMGAMMAS-$- - -- - $-- - - --- -$ --- -- - ----------------------------- ---- $- -_ _ - - - - ---- ---- A FC EET55.-- RADAR RLTMTAST DEV 24.65- - - -- -LINE 11803 I /- -_I IfL11l pfJTIT i1 II TJ1T1[ 0 I-H-I\A ~ _ __ _ _r ---. ~ ,. A . - _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _I-L mrIL0Ua ,~A.NU)_ -Ba-J-JLaI-O]U)wrr-F-a:0I- - - - - _ _ _ _ _ A . -AI-EANSTD EVBI/KMINMAXMEANSTD DEV.000062.599.69016.56.000021.533.2395.678IIcIF-ruF-FLF-cF-LF6agNU.UcF-aLD1wb- r TL/Ki t l lh III i MANXBI/TLMIN .000MAX .9467MEAN .4291STD DEV .1398TOTAL COUNTSCTS/SECMIN 513.5MAX 1376MEAN 841.4STD DEV 168.1POTASSIUM 40PERCENTMIN .104MAX .3241MEAN .1551STD DEV .0492BISMUTH 214EO. PPMMIN .8559MAX 3.435MEAN 1.822STD DEV .4294THALLIUM 208EU. PPMMIN 1.526MAX 9.290MEAN 4.521STO DEV 1.545BI AIR CORED. PPMMIN .5003MAX 1.432MEAN .8454ST0 0EV .2369RESID MAEGAMMASMIN -1219MAX 218.2MEAN -666.1STO DEV 345.1RADAR ALTMTAFEETMIN 333.7MAX 468.5MEAN 389.9STO DEV 21.56LINE .1170-HzU-A-C-ow(U)U)C~3C0Zr 8CmL) psoy + I - --mW~_-- -$ - --- --- -- --"HI-A> _ _ __ _ _ _ _,i.-AJi- - I ij ---- 1--_ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _24 Igal---- -- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -- -- - - -- - - - - - -- --- - -- - - - - - - - - - - - --- -- - -- --- - ---- -|iF?!I_I-m7rD17wb11 09-T1T0118 10IL/ 10 0_LI'zI11A -I ___I7i i flE V I MATL/KI fiIA~LI~1~III4IILJ MINAXE]m m Wrij- -D--L m& -'-L mam 2 oO M-(U\c-O-JL a _H-2:r0If)wL m--- ------ - -------------- K-i----- - - _-$--_-BI/TLMINMAXMEANSTD DEV.000073.7311.1618R.95.000022.563. 1905.456*00001 .026.3339.1177I-UrLCLIarCrn FUUClFC0Ir-NRzUHI- c';WClDCLITOTAL COUNTSCTS/SECPOTASSIUM40PERCENTMIN .0959MAX .2669MEAN .1378SID DEV .0294BISMUTH 214ED. PPMMIN .7351MAX 3.133MEAN 1.612STD DEV .4179THALLIUM 208ED. PPMMIN 1.301MAX 11.63MEAN 4.988ST NEV 1.682B1 AIR CORRED. PPMMIN .4320MAX 1.056MEAN .7631ST0 0EV .1399RESID MAGGAMMASMIN -1065MAX -395.0MEAN -801.96TD DEV 190.1RADAR FCLTMIRFEETMIN 332.6MAX 448.8MEAN 385.3STD DEV 23.21LINE 1160CPa: 9X:___ 1- ________- -___________ ___---- - - - - - - - - - --- - - - --- ----------------- ---- -------------------------------'- f!-1-H- r --- ---- - Z -46 ~ ' ' m E-,- --- -l' ii II--LLe'cri-'--, rD15* m00v 108.31151 151,l6L~g1 l 15011.57V V 10.54T L/KMI___ _____MAX- --- -- MEANII IIST DEVBI/KMINY i IMAX-- MEAN___iM~L~~IF1~MIJI-LmS I-mESN N N 0W 0)) 0)A- -.- -aAF-z0UF-OI-Lart9i:NHU)L-Fa2:h-La. --------- _-- - - - - - -- - J - - -- -- - -g- - - --- g -- - -- - - -$--- - --4--JT-Oa:-L0.00005184. 0000.7199.3211.1258-+zU)z@I.wz::zCc a:0C-)CE:MAXSTD 0EVMEAN 010.8STD DEV 152.4POTASSIUM 40PERCENTMIN .0915MAX .3381MEAN .1431STD DEV .0418BISMUTH 214EQ. PPMMEN .7710MAX 3.188MEAN 1.601STO DEV .3909THALLIUM 208ED. PPMMEN .9628MAX 13.54MEAN 4.746STD EV 1.407L1 AIR COAEQ. PPMMEN .3485MAX 1.305MEAN .7698STDO0EV .1808RESIDE MAGGAMMASMEN -893.8MAX -429.2MEAN -708.2STI) 0EV 68.62RADAR ALTMTRFEETMEN 316.7MAX 470.1MEAN 384.4STD DEV 21.50LINE 1150IN Ior' VIL i "x"~ '.y~V vvvCDUa: U)WH a:--II...- ,.,1BI/TLirJN.ae-'IL o?7t1 11, 1, Ioki/I NAtw' ~ ' e n D19wbm mom9 O5 )6TOT IBM 10 OT -1210 1210 TOT1210 c1 m 10 v v m om N D3 C G _ D V1 \ + " 3 3 m /i\111 El ETL/KMINMAXMEANSTO DEVBI/KMINMAXMEANSTD DEV.000049.4+74.36810.04.000014.10.85792.442BI/TL1. Ol A f M Crz0Lar:- r-0In-ICHHLerpL ),2:LiUIrC 4RT*hmmmm m m mS- - - -. -- -0) 5 5 5 5I"-- -- - - ------- - - -------- - -- -- - -F--*i LsF-.00001.185.2532.2475z-)N 00( wU)0C-)3iMINMAXMEANSTD DEV8Nr1TOTAL COUNTSCTS/SECMIN 128.6MAX 1524+MEAN 483.4STD DEV 247.4POTASSIUM 40PERCENTMIN .0775MAX .58MEAN .2178STDDEV .1393BISMUTH 214EQ. PPMMIN .6103MAX 2.925MEAN 1 .202STD DEV .4451THALLIUM 208EQ. PPMMIN .6760MAX 9.821MEAN 2.851ST0 DEV 1.749BI AIR CORREQ. PPMMIN .0848MAX .5327MEAN .3057STD 0EV .1084RESIDE MAGGA-MASMIN -927.4MAX -208.1MEAN -767.2STD DEV 153.1RADAR ALTMTRFEETMIN 297.2MAX 448.1MEAN 382.7STD DEV 20.20LINE 1210H-01I... _-I----------------------------------------------------------------------------------------------------------------------;; ;Vl IZZ71LsC'Lanm any)"e -70 70I'.,^all-JI aK-JH-H-__ III 4i~hPAtzk! VmnU na sr = mmU) r V~vFiN ESrr.-Lmw0w)0a:L.TL/KMINMAXMEANSTD DEV81 /KNI NMAXMEANSD DEVBI/TLD20wb000064.6415.4016.40.000022.234.2225. 506cJzC"lw-Jowrr0(zmI -C )oU)z-rFIrC hLCI IIEss0nFUGChCCh3ChaWLRm [C-Ea:'-- ------- ---------------------------------- --------rm.r-MMIN .0000MAX .9871MEAN .2105STD EV .1694TOTAL COUNTSCTS/SECMIN 66.64MAX 1566.MEAN 710.2STD DEV 377.1POTASSIUM 40PERCENTMIN .0771MAX .5791MEAN .2053STD EV .0810BISMUTH 214EQ. PPMMIN .7359MAX 4.413MEAN 1.803STD 0EV .6936THALLIUM 208EQ. PPMMIN .7017MAX 9.752MEAN 4.714STD DEV 2.433BI AIR CORREQ. PPMMIN .3004MAX .9671MEAN .5507STD DEV .1496RESID MAGGAMMASMIN -834.4MAX -565.2MEAN -710.6SD 0EV 98.82RADAR ALTMTRFEETMIN 354.6MAX 467.8MEAN 399.4STD DEV 18.76LINE 7009Y1AwtECFClmg ------ - -- --- --iI1ii L ~ LI-I-rII.c.rIu--------------- ---------------------------- -- -- -- --- -- - --- e - - - - - - - - - - - - -TL/KMINMAXMEANSTD DEVBI/KMINMAXMEANSTD DEVBI/TLMINMAXMEANSTD DEV.00055.8313.7614.2118.933.1984.594.0000.8891.1839.1708'MJn M~In 8Lmu3DZ ct3~1mmL .8__-- I LINED21wF N-- I I AA 4111r11NER1zU-JoDcrUC1)zmTOTAL COUNTSCTS/SECMIN 62.53MAX 1699MEAN 657.6STOD EV 399.9POTASSIUM 40PERCENTMIN .0712MAX .4321MEN .2049STNDEV .0719BISMUTH 214EQ. PPMMIN .6923MAX 3.435MEAN 1.697STD DEV .6555THALLIUM 208EU. PPMMIN .6813MAX 11.78MEAN 4.186STO 0EV 2.723BI AIR CORAEU. PPMMIN .3273MAX .8704MEAN .5813STD EV .1521RESIDE MAGGAMMASMIN -858.9MAX -650.6MEAN -773.7STO 0EV 42.03RADAR ALTMTRFEETMIN 332.5MAX 461.9MEAN 386.7STD 0EV 25.01L5d3Uwcc00uJLmmmI a 1 11- 1 I 1 I 1 i-- u l -u i ,EN Dl Dfam OllmNOPIYltmIDca]IP T CtDPI Onm716716 OIDfDICttlonm wwh.OIDDI 1 c0 GomNm w.smNN Qh- amGlDfam-hLiiiii-!! i"o7wzEC710Kr AlIr-0LaF !jNIF--ZflF3L. a _ _ _ _ _ _ __ _ _ _ _ _ _ __ _ __ _ __ _ _ _ _ _ _-Ja:al:al:STD DEV 4081/KMIN .000MAX 27.80M EAN 3.0STD DEV 4.741BI/TLMINMAXMEANSTD 0EV.00001.174.2653.1767z-GmzmsN -ycoew:JZ OH cQHU!)zasD22wbF0HLa-I 1.-."_TOTAL COUNTSCTS/SECMIN 167.4MAX 1785MEAN 782.9STD DEV 397.7POTASSIUM 40PERCENTMIN .0836MAX .5145STD DEV .0862BISMUTH 214ED. PPMMIN .6621MAX 3.881MEAN 1.693STD DEV .7869THALLIUM 208EQ. PPMMIN .7164MAX 11.83MEAN 4.529STD EV 2.80781 AlA CORREQ. PPMMIN .3058MA~X .8420MEAN .5824STD DEV .1254RESIDE MAGGAMMASMIN -1088MAX -599.2MEAN -892.9STD DEV 162.9RADAR ALTMTRFEETMIN 324.8MAX 426.5MEAN 384.8STD DEV 17.71LINE 720aIufI cIIEn FUVI-CII C I-fu.d.W Ir=aC0Lia:a:bz----- ~-------~-~----------I-F-T ji. IIII-MLuLL_____________________________________-______--_-----_---_-_----__-___-fvrulL SfiI S 1TL/K-1.-al-oz(rLrLranm-- I atb GhmOtpemgigiGh2 tpromIpolanm/ 1 pe. uA Ali -D23wbS71 -M7EAN73I~GhmN ptINL. - IST0 0EV,ass11L1 1 31____731(H 731F00E/______________________m BI/KAXSTNDEVHmsI LI~M1 I ~ r ALA AU II.JQO~/ ~pp4A~V~ V V/V VV\~t~J~~ AA~~ J'\AI- -_____1BI/TLMINMAXMEANSTD 0EV0000o60.5016.4115.63.000019.293.7854.845. 0000.8042.1808.1577NzcotLiM --C Daw10zc oUzm-I:uiTOTAL COUNTSCTS/SECMIN M 140.3MEAN 737.0STD DEV 367.8POTASSIUM 40PERCENTMIN .0817MAX .4194MEAN .2116STD DEV .0680BISMUTH 214EQ. PPMMIN .6821MAX 4.505MEN 1 .709S0NDEV .6592THALLIUM 208EQ. PPMMIN .7128MAX 14.82MEAN 4.533STD DEV 2.82881 AIR COAREQ. PPMMIN .2433MAX 1.685MEAN .5819STO DEV .1778RESI MAGGAMIMASMIN -1054MAX -442.1MEAN -875.0SF0 0EV 192.8RADA LTMTRMIN 328.8MAX 454.8MEAN 388.6SF0 DEV 21.05LINE 730a:CJa:a:mlF,310)m-J-J0H:U)0--Ja:Q:Lm-.--.------------ - ------------------------ I--ULI . .I 'IIwrLcaci-JHLmI L[14-JH-NLI N IH fl H AM ____l- _-_--_E9 HIIf tLulf N "'T A1hipN_______r-.JCL- IF-NNLm~NL mar3l:LLIa:L :L-..--- .7 ------- --D24wbTL/KMINMAXMEANSTO 0EV.00069. 1413.6515.52M-Ia1Nzc-f)F-a.,mLiiCEow C-UzU)IIcFEU,aWWacfBI/KMIN .0000MAX 23.99MEAN 3.012STD DEV 4.735BI/TLMIN .0000MAX .8638MEAN .2231STD DEV .1902TOTAL COUNTSCTS/SECMIN 106.0MAX 1493MEAN 640.4STD DEV 296.7POTASSIUM 40PERCENTMIN .0761MEAN .1856STD DEV .0712BISMUTH 214EC. PPMMIN .6985MAX 3.478MEAN 1.421STD DEV .5529THALLIUM 208EQ. PPMMIN .6873MAX 9.612MEAN 3.650STD 0EV 2.0783:.t0al:mC81 AIRE0.MI NMAXMEANSTO 0EV.RESIDE MAGGft'1MASMINMAXMEANSTO 0EVCORRPPM.4176S. 137.6294V .1395-989.7-648.0-891.3100.5RADAR ALTMTRFEETMIN 329.4MAX 414.6MEAN 375.0STD DEV 16.92LINE 740nrYI-- - - - -- --- - - - -------- --- ---- - ----------- --------------7LL m-fl 41 Ia.IrCfCLrl',.ohm,X Oh.m-- I 11I IC 8111 _uanm e0dGIDOIOG1.1 35527. p2 elwm 750 ym750 NNNCl l.ClDlai GM1OIDOI/ \ cnmGlimJtY -mrF-rL. mr.CitF-0LeNF-. m.LrNm mDPO (D AND (m CD Ctom m Av444M_I-VOHw-Ja:a:-a:ma:LmTL/KMIN .0000MAX 106.1MEAN 12.18STD DEV 17.02BI /KMINMAXMEANSTD 0EVBI/TLMI NMAXMEANSTD 0EV000023.843.094.726.0000.9915.2534.1850zU)N , cw0JwUw o,H cuaUCI)zmILINED 2 5 wbTOTAL COUNTSCTS/SECMIN 207.7MAX 2151MEAN 740.9STD DEV 310.2POTASSIUM 40PERCENTMIN .0830MAX .5672MEAN .2142STD 0EV .0934BISMUTH 214EO. PPMMIN 6939MAX 3.512MEAN 1.580STD DEV .5215THALLIUM 208ED. PPMMIN .7415MAX 16.41MEAN 4.353STD DEV 2.37181 AIR CORREQ. PPMMIN .4584MAX .9633MEAN .62STO DEV .7166RESIO NAGGAMMASMIN -848.3MAX -776.5MEAN -902.0STD DEV 44.73RADAR ALTMTRFEETMIN 314.6MAX 473.6MEAN 393.4STD DEV 27.52CUIa:a:I-MINN MIN 6 ownI.-- ^o gM- 29. s ?l.C:az QCL_ 750a.o To .e0(W ' valI D26 bS D~wbL - - jTL/K- - -f- - - ---- j ME N 9.053[ p { BI/LI II,- MA 20.8- - -- MEAN .2- __ _CT_/_ECVj- -MEAN 9.2-STD DEV 32.81v -- - -- - --- MAX 1792m - --------- MIN .0000rD -EA-- - _ - -7 4 . -D E.4 6 3L . __-- -- --- -- -- T ---U2 ~BI/MTH1MIN .0000Lfl cc PTASSIUM 2082 O1 __ MAX 1.2mH- -- -MEAN .26T : -- dL STo DEV .205co BSUTU1_ l _ - --R DAT-- THEALLEUT2-(11- --- _-__CTSSEQ.PPMIN 27300-0- MAX 10.02IQ- g -- -_-_ -- M EANDE 4.82SS1.L Z _ L E. PPM-- - --- - - - - _ _-MTN .98F- ______ ____ MAX .6374- , nMEAN .9815o lSTD 0EV .0135U) r tn - ---------- __ __BISMUTH__ __ _ 214__-z-----F- ~---~MIN -925.9MAX -84.19N ~ ~ - -- B---------- -- B __ --.------------- ___ -B - ___MEAN 1-8930)N- -- - ___- - _S TO DEV 2.357-H- - -- .---------- - - E.PMgMIN .30-\ A. ~MAX 44.32J - - - - - - - - - - - - - -M E A N 3 8 . 8a:-- - --- _______-_____________I q__ _ __ _ __ _ __ _ ___________- - - __ __ BINEIR7CORIPMIN1IfL1Lt ^mMA________ II ii____ tool77 70-im -r 70 MEANvlt-7F-H IAIzUT A[m m mr1Nm DO61NHLe~FiN1 0______ _________________rJC0CBI/TLMINMAXMEANSTD 0EV000052.0811.2811.21.000022.573.3444.261*00001.414.3041.2370NzwDZL 0HCoC7-0zD__ LINED27wbTOTAL COUNTSCTS/SECMIN 343.9MAX 1938MEAN 971.7STD EV 344.8POTASSIUM 40PERCENTMIN .1009MAX .6946MEAN .2802STDNDEV .127uBISMUTH 214EQ. PPMMIN .8782MAX 4.198MEAN 1 .860STD 0EV .6572THALLIUM 208EQ. PPMMIN .7663MAX 11.02MEAN 4.239STD EV 2.30981 AIR CORRED. PPMMIN 1.736MAX 2.430MEAN 2.038STO 0EV .1853RESID MAOGAMMASMIN -881.1MAX -818.9MEAN -855.8sro 0EV 19.57RADAR ALTMTRFEETMIN 332.7MAX 453.2MEAN 397.0STD DEV 19.73auccahcFn FUUClC0FFUc20UHCH FLJL.. 1-mLCtIr770-~ . D28wb4---_MAX 66.61SMEAN 13.73STO 0EV 13.57BI/KMAX 28.15MEAN 3.7387 S m ot70 7 a X-I/TLMIN .0000MEAN 23STD DEV .1675C!)TOTAL COUNTS-CTS/SECMIN 000MAXC157-In STD DEV 4122MIN .2000MA]-X .701ENMEAN .244Z- STD DEV .1675r m BISMUNI2Tr~N p TPOTASSIUT-) EM.N PP 4Q]MEAN 10.2F- STD DEV .162WDE _cPERCEN--HA U 20HUQ MIN .879MAX .5193l MEAN .2444STD DEV .599am moco THALLUMH21E.PPMMIN G.16MEAN -. 76STD DEV 2.540LCMAX 11.156ST0EV 2.106C -MAX -8.6Q RASDRAMRCEMEAN 387.2--- STD DEV 20.29---- ---- ---- --- ---- ---- --- - - -- - ---- --- ---- ---- ---o1PP.a..N Vwwm y90 790 -,aces 790 790 YesQIPOIOWOhmahsoff.ohm aft.J_HrIL-ChICFCaFC12FII 8 ki l). W 1 11 -%A .v111I~~ -4W -JI IILI___MAXMEANSTD 0EVBI/KMINMAX]iiSTDDEV12nrn Nzn t0-I c MA~A AAJm~J:a:Lm.000076.0110.8011 .82.000025.782.5333.897BI/TLM1IN .0000MAX .7583MEAN .2207STD DEV .1789TOTAL COUNTSCTS/SECMIN 171.6MAX 1851MEAN 783.0STO DEV 350.0POTASSIUM 40PERCENTMIN .0864MAX .7236MEAN .2745STD 0EV .1177BISMUTH 214EQ. PPMMIN .7205MAX 3.967STD 0EV .6466(THALLIUM 208ED. PPMMIN .7020MAX 11.48MEAN 4.206STD DEV 2.373BI AIRMINMAXMEANSTD 0EVCORRPPM.59301.293.9451.1680RESID MAGGAMMASMIN -882.2MAX -742.8MEAN -794.7STD 0EV 30.36RADAR ALTMTRFEETMIN 307.7MAX 463.0MEAN 384.3STD DEV 24.64LINE 790D 2 9wbaNzUf)mwwCOUza0UH F8--~N ,. _,Eg I tq I n HmE3 Ir-g-~w?\/ v v--i.arr I 1rrOHWrqwLr__STL/KI I 4 M TMINt ]WAJI*1L.I-ftJH.Al i1 V11 A.-LoII i'z0L sCE:F4~NrN-JJL3fC9:3racc:Q:ccTL/KA MIN .0000MEAN 11.78STD DEV 11.0581/KMINMAXMEANSrD 0EVBI/TLMINMAXMEANSTD DEV.000017.912.7663.725.0000.6291.1987.1867zUf)z~m w-JaWcrc,J ::DQUHmlD30wb.TOTAL COUNTSCTS/SECMIN 85.55MAX 1816MEAN 684.2STD DEV 315.8POTASSIUM 40PERCENTMIN .0777MAX .58MEAN .2363STD DEV .0829BISMUTH 214EQ. PPMMIN .7429MAX 3.385MEAN 1.512STD DEV .4339THALLIUM 208EQ. PPMMIN .6978MAX 13.29MEAN 3.577STD DEV 1.874BI AIR CORREQ. PPMMIN .5583MAX 2.830MEAN 1.077STD DEV .7104RESIDE MAGAMMASMIN -858.6MAX -699.1MEAN -769.7STD 0EV 43.59RADAR ALTMTRFEETMIN 353.5MAX 445.3MEAN 396.7STD DEV 16.77LINE 8000m .[LaLIii Iif...vo. iGlrlolo"I -il1[ i I trl-l r----im.IN:tf.WtMLmN \= ah.Chin YIM mOhlCM11OMniD 31b11 v 811 o n; po nNisF9-J{-mLsJH.TL/K- MIN- -INMAXI-1~ MEANIII STDO EVImLmrUOF sm m.-4m9rNiJ mNL m~ _____11L9- - - - - - - - _ - - - r _ _g - - - - - -E--4zCoe zc ,ww rr C)Z O~_)1-iCo)zmBI/KMINMAXMEANSTO DEVBI/TL.00082.199. 87411.19.90022.762. 1523.532MIN .0000MAX .8730MEAN .2040STD DEV .2045TOTAL COUNTSCTS/SECMIN 86.43MAX 82189MEAN 671.9STD DEV 357.8POTASSIUM 40PERCENTMIN .0766MAX .5651MEAN .4STD DEV .1167BISMUTH 214ED. PPMMIN .7177MAX 4.424MEAN 1.582STD 0EV .5571THALLIUM 208ED. PPMMIN .6760MAX 16.39MEAN 3.557STD DEV 2.143BI AIR CORREQ. 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PPMMIN .1193MAX .6118MEAN .2961STO DEV .1084RESIDE MAGGAMMASMIN -915.5MAX -588.8MEAN -803.1STO 0EV 98.98RADAR ALTMTRMIN 309.1MAX 456.4MEAN 389.0STD 0EV 28.08I CahChII6fN FUUahCaI rI-I-fuaWi=aEf0:H .F0:Q:L:_.13 r r r in It I II III ufl r r it Y - 5 r Y Y t I It - V If YII ,V- I I I f Wf 11_ ulna t r r .y r~ _ Y v- r'^ r -vti--------- -------- --------------------- - -- - --- - - aL BGIrII f- r 5ran IFrrfmns7zCh[8-JLmKo-1D 3 3 wb1-+ILmCJ rFLmFI-J-NZ:HcoLiIrLm '4-m-------------------- x--- -TL/K(MINMAXMEANSrD DEVBI/KMENMAXMEANSTD DEVBI/TL.000064.8915.4814.52.008019.25'4.422'4.782MIN .0000MAX .9512MI0E .86eJzS Z&-cow1 0z-JoLUCE cEZ c-J-]zDm-NTOTAL COUNTSCTS/SECMIN 222.1MAX 1741MEAN 805.7STD DEV 381.4POTASSIUM 40PERCENTMIN .0814MAX .5407EAN .2553STD DEV .1086BISMUTH 214EQ. PPMMIN .6685MAX 3.790MEAN 1.731STD DEV .6630THALLIUM 208EQ. PPMMIN .7439MAX 12.61MEAN '4.607STD EV 2.706BI AIR COAREQ. 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S. DEPARTMENT OF ENERGY6 - 83 00 -- p -',83 0030 [{ X 1. 0a o OM=o&ooo 0w8200ococooo n 00 _ _ao Qo 0o 000 0 0 fi :0 o ao oa a o cmoc CC0000000 0000 O0 00000" 00 O ooo, , oooo 0000000 00 , o0x 00 0 p0 C0p0 0000000000000000g 00" ". .. .. ." 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HoYTHLLS_ E~ia ACxsoHYvLL- FLA_ 18e' as hw o hi umaevlatTHORIUM/POTASSIUM STANDARD DEVIATION MAPMISSISSIPPI / FLORIDA PROJECTU. S. DEPARTMENT OF ENERGYI C b00000~000 000 00 0 0000BO00032 00>OOOOOOOOOOOOOOOOOCDOI3--'P e, 00131 30 H {31 30 1310082 01 80 001 000000000000 0 000000000 0000 0 0082 0032 000800 co).0000 0000 0000000000 000000000000000000000000000000000000000o 00000000000000o 0000000000000000 0o 0 0 00 000 0000 6 T000000 0000000000 0 00000000000000 0 00 0o000 0"000000000000000000 :00 080o«>Oo0 00 00 00 0o000o o00 CT 00o 0 0000p)A 00 080 0000 0000 00COO 000 0000000131 0080 0SURVEY ANDCOMPILATION BYGEGG GEAMETRICS00000000000c 00000oo0 0 0.... 880INDEX TO ADJOINING SHEETSGEORGIAVALOSTR H 7 STES ON $A88 -]J 8838 A0 - DATA STATISTICALLY ADEQUATEBLANK- DATA STATISTICALLY INADEQUATE" - 1 o ABOUT MEASURE OF CENTRAL TENDENCYNOTE. ON E -W LINES. +e TO NORTH, -O TO SOUTHON N - S LINES, + TO WEST, -O TO EASTURANIUM/POTASSIUM STANDARD DEVIATION MAPMISSISSIPPI / FLORIDA PROJECTU. S. DEPARTMENT OF ENERGY000000000000i0 0 0BRUNSWICKt80I0 00 000 000 0 0000000 0.000800 0 000008E1bob0 0 00800o &00000 000008000 00 000000000000 0000000000000.704 on ao c0 00 0080 8 0 0 0SCALE 1:500,000I--- -., _- -80 00_ 32 00100000{31 30131 30 -0131 ooLIBRUNSWICK20000 0000000000 0 000000000 0000000 00S2 20 O 2O0000 00000000000000000000000000000 0.S0 0 00o000000ooooooooooooooooooooooooooooooooa:o.: r...22... 2222 2 ..2.20 ....02 2 22 222 2 2oooo 2 2 2 222 2 22 22 o 2 oooo 2ooooooo 22o 2 2ooooa20o000' 00 000 00 0 000000000 0000 0000200 000000000 00 000 00 0 00 0 0 0 0000 0 0o00000000000000010000 ; 000 0 000000000000000001oooo 00000000 000000 0008 -8® . . 2200oooo oo o o o om c00000"00o 00 00000 Jo.00 00 0 0 000000000o0 00 0000000000-.000- 0oo oosoo~ooa0 0"0000 00o00010 0 0 0000000 0000 0e00SCALE 1:500,000MIE 0U.,, _URANIUM/ THORIUM STAND000000000oooooo0ooo0000 0.2.2.8o - DATA STATISTICALLY ADEQUATEBLANK - DATA STATISTICALLY INADEQUATE.- 1 O A80UT MEASURE OF CENTRAL TENDENCYNOTE: ON E - W LINES, +o TO NORTH, -O TO SOUTH.014 N - S LINES +o TO WEST, -o TO EAST,INDEX TO ADJOINING SHEETS .SAVANNAH - - 3MAC N 111, JAMES t- NOGEORGIA__ AC~NS ViLtVALOOSTA H 175 STETSON TMESAN FLA -o.14- e e~cm sono s o ~ a ao.ARD DEVIATION MAPMISSISSIPPI / FLORIDA PROJECTU. S. DEPARTMENT OF ENERGY82 0032 00000O O000000000000 00 00000000 0 00000 m0cnooo0oooo000000000 08..000 0 000 0 00E120 0000000000000000000000SURVEY ANDCOMPILATION BY1'*EGG GEa4ETRIS.- --. --31 30APPENDIX F - Histograms and Map Unit ConversionTableNTMS NH 17-1/2 'RYCROSS/BRIJNS/I CK MAP UNIT ORL TOTAL NUMBEROF SAMPLES1280iia0:0108030.000THORIUM0 EQUIVALENT PPM 15 . 0MEAN /DEUTEMEDRN 5.. 5M3308 PLEU/K7. 85 7 . 20 0 2273 SAMPLE3108L)zwi0027 400MERNMEDIRN2..0000.340 0.320 300 EURANIUM, . , ,A n n0 EQUIVALENT PPM 5 . 0MEAN /T-MEDIAN 1.-9 1.- 8 30093ADEUATPEU/THPOTASSIUM113Uzi088Uz00ME RNMEDIRN 24.F33950.00023.000 2477 AsEOURTEFwb3312r0 EQUIVALENT PERCENT 1- 0A 0.3 0.2 2477AAETH/K0MEAN rMEDE RNRb.LNTMS NH 17 - 1/2 RYCROSS/BRUNSVICK MAP UNIT OS TOTAL NUMBEROF SAMPLESTHORIUMEQUIVALENT PPM1 1.80MEAN /MEDIAN 5.567 4.800URANIUM15.048 RO"jN30.000SAEOURTEz0wLL0 EQUIVALENT PPM 5 . 0MEAN/MEDIN 1 .0 1 . 0 1 q ROUTEUa/TH0MEAN /MEDIAN 0 .517 0.4I203W0W02.000ADEQUATE1 SAMPLESPOTASSIUM0 EQUIVALENT PERCENT I . 0MEDIAN 0.2 0.2 27 ADEOULESTH/II - - _____________________.._____________________0MEAN /MEDIAN50.00013.700 12.500 27 AMES49F 2 wb0MERN /MEDIANWMd030U]" INTMS NH 17 - 1/ 2 AYCROSS/BRUNS-WICK MAP UNIT : OHM TOTAL NUMBEROF SAMPLESTHORIUM179z0450 EQUIVALENT PPM 1 5 . 0MEAN /MEDIAN 2.8 2.1 2672 AAMLU /K"" r nn "16.203 5.70085030.000779 SMPLE0MEAN tMEDIAN 0.30 0.3402.000850 ADEQUATE- -r59z0iiL.0URANIUMK0 EQUIVALENT PPM 5 . 0MEDIAN 1.3 1 2 880 ADEQUATEU/THF3 wb2883174U-zLii0isLi-01826000MEAN /MEDIAN0MEAN /MEDIAN 12-56050.00010.000 2520 6AEOUTEPOTASSIUM0 EQUIVALENT PERCENT I . 0MEDIRN .2 0.2 2602 ADAMPLESTH/Kr. . . . .NTMS NH 17 - 1 /2 IRYCROSS/BRUNSWICK MAP UNIT : OHITOTRL NUMBEROF SRMPLESTHORIUMII70Wi'1 1I0 EQUIVALENT PPM 1 5 . 0MEQRN f - /0 C R']EiJIJRTEMERN/ -, 2 - USRMPLEU/Kj1i pHpp7Uzir05.004 4.8007uzL030 .000R6OURTE7b SAMPLESURANIUMF[1 rj J11K0MERN /MEDIAN 0.305 0.2802.0002 RDEQUATE52 SAMPLESI7008Uz0L0 EQUIVALENT PPM 5 . 0MERN /DQUTMEDIAN 1 3 .52 RSAMLEU/T HPOTASSIUM0 EQUIVALENT PERCENT 1 - 0MERN Ai ~ REUTMERN 0 -2 0 .2 T HRM/LEKTH/K~0MERN / 3.t4MEDIAN 1L3 5 5L4 11.00050 .00087 REUTIIF4 wb1000FLi- I0MEN /MEDIANIliI IlN T MS NH 17 - 1/2 VAYCROSS/BRUNSWICKTHORIUMEQUIVALENT PPM5.7MAP UNIT11u015.0ADEOUATE1 5 3 SAMPLESU/V9.330 3.00011Lizwd0030.000AOEQURTEQTSBTOTRL NUMBEROF SRMPLESURANIUM11hL _0MERN /MED IAN 0 .308 0 .300F5wb153-F2.000ADEOURTE122 SAMPLESPOTASSIUM8Uz0W00MEAN / .)OMEDIRN 2 14 4 19.5000 EQUIVALENT PPM 5 . 0MEAN / 6 1 22 ROEQUATEMEDIAN-1 H AMLLI/ THF'R_FFSUzwd0W24f0'1l0 EQUIVALENT PERCENT I . 0N 02 0.2 110AMED NTH/0MEAN /MEDIAN50.000110 ADE6U005.40|ERN /MEIIN-- T-IVfNTMS NH 17-1/2 RYCROSS/BPUNSVICKTHORIUM' " !32GUD8_ n ";n n nMRP UNIT :QUTPRRM18UzWL0WiOZ-LL00 EQUIVALENT PPM 15 . 0MERN/ LK34 q2 DQUTMEDIAN 4.3 3.4 43Q IMPES1L[I -9.4L42 7.50038UzwiW3030.00011 2 RD%2f!TOTAL NUMBEROF SAMPLESURANIUMI1F6 wb439LPL f0 EQUIVALENT PPM 5 .0MERN /.7 . 2 AD EQMEDIAN I7' 2 EQUU/THE1 , ,0MERN /MED ERN 0.335 0.32023uz002.000288 ?%0POTASSIUM20Uz000MERN /MED IRN50.00027. 58 22.500 17j IPL0 EQUIVALENT PERCENT 1 .0MERN .2 0.1 171 ADEQURTETH/MPLESNif JLFLP]fl nr~P0L0MERN /MEDIANLd 1n a ririLIITnfl n i MllN TMS NH 17 - 1 /2 VAYCROSS/BRUNSWICKTHORIUMMRP UNIT OTPRRIURANIUMTOTAL NUMBEROF SAMPLESF7wb356POTASSIUM0 EQUIVALENT PPM 1.5 . 0"EDIRN 4 . 6 4-. 0 3 5 8 RSRMLElU/KMED R 4 L~0~5 REULT0MEAN /MEIIAN 9.238 8.70033UzwiD030 . 0001 37 RSRMI)I15LUzwi0L00MEAN /MEDIAN14UzbwDOi0 EQUIVALENT PPM 5 . 0MERN /RMEDLRN I-I-L. 274 ADERMPEU/ TH-- T2.0000.335 0.320 274 AESTE26UzC+:00MEAN IMEDIAN 26.877 22.00050.000162 ADEQAE10J Itfqq Hl0 EQUIVALENT PERCENT 1 . 0MEANA /-q~DQITMEDIAN 0.2 0 H.9/KSAMPLES~TH/jinn.rjL1L~[1D0Lit oNTMS NH 17 -1/2 WRYCROSS/BRUNSWICKTHORIUMMRP UNIT125W0131UzWi0Lii00 EQUIVALENT PPM 15 . 0MERN / n i o -QrK 7 EO2URTEMERN -.0 5 . 8. 337 f RMPLE9U/K0MERNMEDI RN30 .000403UzL-07.94 7.200 2858 RSRPRLOTPRM TOTRL NUMBEROF SRMPLESURANIUM122UzWi000MEAN /MEDIAN2.000ADEQUTEF8334064POTASSIUMV10MERN /MEDIANblft151Uiz00Li.00 EQUIVALENT PPM 5 . 0MEF;N / 1JE0UR0E"iE|Nr N1. - 1 - 8 3087 "'9RtLEsU/TH-L[PdI I50.00025.143 24.000 3018 SRALE0 EQU-VRLENT PERCENT I .0MEDIAN 0.3 0.2 30 RSRMPLESTH/K.u_nnNTMS NH 17-1/2 AYCROSS/BRUNS'SICK MAP UNIT : OTPAI TOTAL NUMBEROF SAMPLESTHORIUM URANIUM POTASSIUM0 EQUIVALENT PPM 15 .0MERN /MEDIAN L4.7'4.3 207U/K3010.808 1 0.800U1f.0006911LJW11w~zwd02020zwi0012UizwiW00MEAN /MEDIAN 0.315 0.30011z002.0001 ADEQUATEI 46 SAMPLES0 EQUIVALENT PERCENT I .0MEDIAN SAMPLESTH/K0MEDIAN 27 . 1'41 22.5000 EQUIVALENT PPM 5 .0MEAN / 7ADEQATMEDIAN -f 16 1 4bSUMPL/ESU/TH207UKIifF 9 wbfill"[1' 0MEAN {MEDIAN50.000108 ADFLEEIIfl 1J '1T117 - 1 /2 YCROSS/BRUNSVICK MAP UNIT : TTM TOTAL NUMBEROF SAMPLESFl 0 wb870THORIUM----43>-zLi0i2000 EQUIVALENT PPM I5 . 0MEAN 9 3.3 667M1ED IARN U3./U/1MEAN /MEDIAN 8.080 7.50045z030.000293 ADEQUATE, ,0 EQUIVALENT PPM 5 . 01 .8 1 .3 477 ADEQUATEU/THURANIUMIIYdRfJLF23UzWLi0MEAN /MEDIAN 0 .398 0.34012Uzwi0LiL02.000478 ADEQOTE7/ AMPLEPOTASSIUM25U'zwi0Li- LiKJI.4lri 1IriBII0 EQUIVALENT PERCENT I .0MEAN 0.2 0. 2 3 42 PETH/II0MEANNMEDIAN 25 .834 23.50050.000342 ADELENTMS NHLn0 nf FLr-IDiNT MS NH 17-1/2 VAYCROSS/BRUNSSICK MAP UNIT OTTI TOTAL NUMBERURANIUMTHORIUMEQUIVALENT PPM2.7 2.215 _A PE28jEIJUIVALENT PPM1.2 1.00MEAN /MEDIAN5.02 4L A6POTASS IUMJ v0-0MEAN /MEDERNEQUIVALENT PERCENT0.3 0.2 1.058 DOR EU/ku1'6.533 6.00030.000f. 9 ADEUATET SAMPLES230MEAN IMEDIANU/TH0. 18 0..38082.0002'43 AEUTTH/KUI00MEAN/MEQEAN 21-001[0.000 0 00 584f30uzWiLL.F11wb0MEAN /MEDIANzLCIL0UizIL00MEAN /MEDIA ANrJu3rwZi IIIlrLLr'NTMS NH 1 / -1/2 VRYCROSS/BRUNSI ECK MAP UNIT OTPEM TOTRLNUMBEROF SAMPLESTHORIUM58UzUV1IL012UzUi0Uia:L00 EQUIVALENT PPM 15 . .0MERN 4 . 1 4. .0 ; ROEIPRTEMEDEN I ;DU SAMPLESU/hKL9.875 9.60030.00025 6 "REOEURTE2 5 )SRMPLESUi1386LUz00URANIUM78zbli0Wiac:LI00 EUIJ IVRLENT PPM 5 . 0MEAN: f ROIIJRTEMEDRN 5 1 .4 1 4 1 1 RMPLE:U/TH[125L)z0IL00MEAN fMEDIAN3L4LizWi0L02.0000.384 0.340 1408 SAMPLESPOTASSIUM0 EQUIVALENT PERCENT I . 0MERN0.2 . 1 2_SMPLESTH/K0ME ANR 32.23250.00028 .500 2868 SRMEF12 wb1693FinIiLILlld4frflflIrTT2l rJllfl- -T1IL'd0MERN /MEQEIRNlipkurL uir jLjnLHrL',V111nTNTMS NH 1 7 - 1 /2 VRYCROSS/BRUNSVICK MAP UNIT OTPEI TOTRL NUMBEROF SRMPLES52Uz0L01007.952 8.400THORIUM0 EQUIVALENT PPM 15.0MERN /MEDIN 31 2 7 OOOASAMTLESu/K42UzWi030.000118 RDEOURTEURANIUM[Jz0iLL0MEINNMEIEN8Uzi0 EQUIVALENT PP ' 5 . 0MER N 1.2 1.1 553 9RMPLEEU/THK - L2.0000. 371 0.340 553 SRMPLESPOTASSIUM0MERN /MEDIAN 27 .161 27.000F1 3wb95526zi0L[ HrffLAn0iiI0MERN /MEDE RN50.000192 ADEOURTE0 EOUIVRLENT PERCENT 1 - 0MEDIN /.1 0.1 192 ROEURE" -N- -__f1INTMS NH 17 - 1 /2 AYCROSS/BRUNSWICK MAP UNIT QTWM TOTALANUMBEROF SAMPLESTHORIUM1010z0160 EQUIVALENT PPM 1 5 . 0MEDAN 33 8 8 ADEMEDIAN0MEAN/MEDIAN 9.6GIG 8.70030. 0002G7 ADEOUTEr1VI1ry~~~LJ lLP .0URANIUM0 EOUIVALENT PPM 5 . 0MERN/ J i 11L i . RDtOQURTEMENrRN 1-.5 1 .- 3 1 23 1 PLE'U/THz0LL.010700Uzwi0OiWi02.000MEAN ADEQPEPOTASSIUMUZWdQWiLi..00MEAN/-MEDIAN2 8 .235 27.00050.000331 ADEQJRTE219219F1 4 wb0 EQUIVALENT PERCENT 1 .0MEANAN 0.2 0.1 335 ADEQUATE/ SAMPLESTH/0F r,nnNTMS NH 17 - 1 / 2 AYCROSS/BRUNSVICK MAP UNIT : TWI TOTAL NUMBEROF SAMPLES87u6LL05Uzw0Wd0MEANMEDIAN 8.2 1 6 6.400THORIUM0 EOUIVALENT PPM 15 . 0MERN REMEDIAN 1.6 1.3 580 APU/K13UzL030.000ADEQUATE2- SAMPLESURANIUM44~UzL00MEAN /MED IAN 0.609 0.5402.000238 ADEQUTEG38SAMPLESIFPOTASSIUM12uz0ii00 EQUIVALENT PPM 5 . 0MEDIAN 0 .9 0 8 277 SAELAEL/TH18 .'32 18.50050.0004 ADEQUATE7 7Fl 50MEAN /MEDIAN0 EQUIVALENT PERCENT I - 0MEANTAEREMEGAN 0 . 10 .1 48 SAMPLESTH/K"nNTMS NH 17-1/2 'SRYCROSS/BRUNS/ICK MAP UNIT QTPPS TWTRL NUMBEROF SAMPLE STHORIUM1081036Uz00MENMEDIAN 1 0392 99030.000668 ROEQURTEii6 03UzU0387Uz000 EQUIVALENT PPM 1 5 . 0MERN /A DQURMEDAN C I.?IIqU/AUKMERN /MED IRN2.0000.80 4 0.560 9883 "SRMPLEPOTASSIUMURANIUML-168uzwd0Lii030uz022 .830 21.500F16wb0 EQUIVALENT PERCENT 1-0ME=IN / FIDEQURTEMEDIrAN 0 .1 0.1 8 H /RMPLESTH/KF AJ01,0 EOUIVRLENT PPM 5 . 0MEN / - 1 970A RDQLTEMi"--LELi/T123810MERN /MEDItRN50.000860 oEORrEI -n-- - srir f.- - ' . .NTMS NH 17 -1/2 YCRO S/BRUNSVICK MAP UNIT : TPMU TOTAL NUMBEROF SAMPLES696Li02160MEAN /MEDIAN30.0001 0. 551 10.200 616 8SAMPLESTHORIUM0 EQUIVALENT PPM 15.0MEAN/ AEQUTEMEDAN 4.9 4. 818 672 SRMPLE9U/K0URANIUM720L)iz0014740 2.0000 EQUIVALENT PPM 5 ..0MEAN/MEDIAN a -8 1 .7 17768 SEULLEL/THPOTASSIUM~10 EQUIVALENT PERCENT I . 0MEDIAN 3A UTH/KUL-0'466Uz050.000MEDIAN 0 .381 0. 360 17767 SAMPLES MFl7wb18673000 . .1 . .I , . I .EDIN 2.4 32 0 0 8484AS MPLUNTMS NH 17-1/2 VIAYCROSS/BRUNSVICK MAP UNIT TMH VOTL NUMBEROF SAMPLESFl18wb1358THORIUM850014L-MED"RN 11 -781 11.70030.0002 ROURTETiURANIUMMEAN /MEDIANII 71Uz0122L)z0iiU-0"I n n n '0 EQUIVALENT PPM 15 . 0MEAN 4.2 4.0 135 RO EU/K2.000POTASSIUM04E . 0 0 13-4AQURTE MERN / 33.092 32.50050.000287ROURTE-.J0 ErUIVRLENT PPM 5 . 0MERN / -.71. 13 ROEURTMEDIAN I / T -. b I 33 SAMPLEHSU/THK-000012GOUz0Wiof:U-.0U-zWi0WI--Ul0 EOLIIVRLENT PERCENT 1 . 0MEL"RN 0.1 0 . 2TH/SRMPLEST H / [I 1 I T iNTMS NH 17 - 1/2 AYCROSS/BRUNSWICK MAP UNIT : TMM TOTAL NUMBEROF SAMPLESTHORIUM227zLi050uiz0IA.00 EQUIVALENT PPM 15 .0MEA ROUTEEDIN .2 4.0 5633 SAMPLESU/K0MEN 130.000ROEOURTE362z0ii0-Jij0MEAN /MEDIAN2.0000 .425 0.400 5464 ASRMLES260iUzWi~10WiLi-0RTJYJb0MERN 36. 00050.000A 1033RURURANIUM1F19 W b5G33217uiz0IL-0152Uz0WiU-00 EQUIVALENT PPM 5 . 0MEAN/MEDIAN 1.6 1. 5tW4 ROE'IJATEU/TH_POTASSIUM0 EQUIVALENT PERCENT I . 0MEDIAN 0.1 0.1 1038 SAMPLESTH/KNTMS NH 1 7 - 1 / 2 VRYCROSS/BRUNSEICK MAP UNIT TOSTOTRL NUMBEROF SRMPLESTHORIUM71U-zw~0LIL-0-. -.053L)z0015.0O1 AEURTE90 RMPLESU/K10.50081I030.000130 RDEQURTEURANIUM1L0tEIN tMEDIAN 0.408 0.400[V2.0002UOEOJRTE80 SAMPLESPOTASSIUMK1Kdl0MERN /MEDIRN 30.201 29.50087133V-z0LI010zILl00 EQUIVALENT PERCENT I . 0M N -7j 0. 1 152 AEQUATETH/K[kt-F 20wb0MEN /MEDIANEQUIVALENT PPM80U U0MERN/MEDIAN 1 0.3 2 40 EOUIVRLENT PPM 5 . 0MEN M1A-1-C USRMPLEU/TH. ., I " Ii50.000152 DEQUTENTMS NH 17-1/2 AYCROSS/BRUNSVICK MRP UNIT TETOTAL NUMBEROF SAMPLESTHORIJM-951UOILi01403011.829 11.00nr-.000289 2 AURANIUM5GUZLir076UOWiW:L00MEAN /MIED IANz0ir0L2G.0000 .355 0.340 854 SAMPLESPOTASSIUM0ME RN 37 .672 37.5000 EQIJIVALENT PPM 1 5 . 0MEDIN 5.0 T.8 818SU/K331 2F21wb920pul o n ri0 EQUIVALENT PPM 5 . 0MN /- ~ - DQUTMEDIN 1 .7 1 . 6 85 RDR SMPLESU/TH4 4UZL00MEAN /MEDIAN0 EQUIVALENT PERCENT I - 0MEAN / 02 01 334ADEUATETH/K50.000TF22wbWAYCROSS AND BRUNSWICK QUADRANGLESComputer Map Unit Symbol Conversion TableComputer MapUnit SymbolQALQSQHMQHIQTSBQTPRAMQTPRAIQTPAMQTPAIQT TMQTTIQTPEMQTPEIQTWMQTWIQTPPS*TPCDTPMUTMHTMMTOSTEOGeologic MapUnit SymbolQalQsQhmQhiQtsbQtpramQtpraiQtpamQtpaiQttmQttiQtpemQtpeiQtwmQtwiQtppsTpcdTpmuTmhTmmTosTeoOn the following pages, histograms for each computer mapincluded in the same order as they appear on the above list.unit areGeologic descriptions of original geologic map units are in AppendixA.Areas over water or cultural features were assigned separate map unitsymbols and were removed from the data block during processing.*Statistical analysis was not performed on these units due to there beingan inadaquate number of samples.NOTES:APPENDIX G - Uranium Anomaly Summary andStatistical TablesANOMALY SUMMARY TABLEANOMALY FLIGHT COMPUTER MAP UNIT AND NO. PEAK1 C2 C3 C4 C5 C6 C7 C8 C9 C10 C11 C12 C13 C14 C15 C16 C17 C18 C19 C20 C21 C22 C23 C24 C25 C26 C27 C28 C29 C30 C31 C32 C33 C34 C35 C36 C37 C38 C39 C40 C41 C42 C43 C44 C45 C46 C47 C48 C49 C50 C700700700700700710710710720720760760760760760760770770770770770770770770770780790800800800800800800800800800800800800800800800800800800800810810810810ANOMALOUS SAMPLES IN UNITTMMTMHTMMGALGTPAMTMMTMMTMHTMHGTPAMTPMUTPMUGTPPSQTPPSGTPPSGTPAMTPMUTPMUTPMUTPMUQTPPSGTPPSGTPPSGTPPSGTPAMQTPPSGALTEOTEDTEOTPMUTPMUTPMUTPMUTPMUTPMUGALGALTPMUTPMUTPMUTPMUTPMUGALGALTPMUTEOTOSGALGAL/ 3/ 1/ 5/ 3/ 1/ 1/ 3/ 3TMM/ 2TMM/ 3/ 3/ 5/ 5/ 1/ 4/ 3/ 1/ 3/ 2/ 1/ 1/ 3TPMU/ 2/ 3/ 1/ 1/ 3/ 2GAL/ 2/ 1TOS/ 1/ 1/10/ 2/ 1/ 2/ 4/ 1/ 2/ 4/ 4/ 2/ 2/ 4/ 2/ 1/ 1/ 3/ 3/ 1PPM3.03. 02. 43.23.92.72.92.52.23.72.83.02. 12. 52.03.33.23. 13.63. 12.32.22.01.83.82.23.82.82.72. 53.23.33.83. 53.23. 53.94.33. 53.32.83. 13.43.84. 13. 53.82.23.84. 6NUMBER OF SAMPLES WITH ASTANDARD DEVIATION OF :1 20 2O O3 21 2O OO O1 12 22 11 12 14 13 2o o3 11 2O 01 2O OO 0o O3 10 22 1O Oo o1 12 2o 24 5O 00 01 30 00 O0 10 30 00 00 22 20 2O O1 20 10 0O O2 12 O0 07 GT70 0O 00 00 00 0O 00 00 O0 00 o0 0o 00 0O 0O OO 00 O0 00 00 0O 00 0O 0O 00 0O 00 0o oo 0o 0O 00 00 00 00 o0 00 00 00 00 00 0o 0o 0o 00 0o o0 00 00 00 0G1wbANOMALY SUMMARY TABLEANOMALY FLIGHT COMPUTER MAP UNIT AND NO. PEAKANOMALOUS SAMPLES IN UNIT PPM51 C52 C53 C54 C55 C56 C57 C58 C810 GAL810 TPMU810 TPMU810 QTPPS1150 TMH1150 TPMU1170 TMM1170 TMM/ 1TPMU/ 2/ 4/ 1/ 1/ 1/ 2/ 1/2/0/0/0/0/0/0/0/0/0/0/0/0/0/0/02. 62.82. 72.62.93. 12.82.9NUMBER OF SAMPLES WITH ASTANDARD DEVIATION OF1 2 3 4 5 6 7 GT72 1 0 0 0 0 0 00 2 0 0 0 0 0 03 1 0 0 0 0 0 0o 0 0 1 0 0 0 00 0 1 0 0 0 0 00 0 1 0 0 0 0 00 1 1 0 0 0 0 00 0 1 0 0 0 0 0NOTES: M INDICATES THAT THE ANOMALY LIES OVERA URANIUM MINE OR PROSPECT.C INDICATES THAT THE ANOMALY LIES OVER A CULTURAL FEATURE.W INDICATES POSSIBLE INTERFERENCE BY WEATHER PHENOMENA.G2wbMAP UNIT GALPOTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDIST-0. 1502-0.2331-0. 6126-2. 63650. 0332-8. 4434-2-0. 00470. 48971.44750. 86030. 13552. 4842-10. 14081. 21253. 50764. 35710. 237813. 411800. 28631.93535. 56777. 85390. 340124. 3394+10.43182. 65817. 627811.35070. 442435. 2670+20. 57733. 38099. 687914.84750.544746. 1946+30. 72284. 103711. 748018. 34430. 647057. 1222MAP UNIT OSPOTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDIST0. 06860. 4820-0. 51620. 2624-0. 25411. 45720.17751.03672. 05515. 56730.517213. 6999+10. 21381.22162.91227.33560. 774317. 7808+20.25011.40653. 76939. 10391. 031421. 8617+30. 28641. 59144. 626410. 87221.288525. 9426MAP UNIT OHM-2 -1POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0. 0235-0. 1709-2. 1310-2. 3058-0. 0267-10. 1061MAP UNIT OHI-2 -1POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0. 0375-0.3931-4. 0181-1. 68170. 0365-13. 9962MAP UNIT GTSB-2 -1POTASIUMURANIUMTHORIUMU/KU/THTH/KDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMAL-0. 0074-0. 2714-1. 4634-4. 44280. 0470-29. 22010. 06370. 40840. 81630. 14830. 1340-10. 0987MAP UNIT GTPRAM-2 -1POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0. 0449-0. 8618-4. 7093-6. 14170. 0964-30. 41470. 0275-0.0225-1. 7036-0. 94700. 1760-11. 0573-3NORMALNORMALNORMALNORMALNORMALNORMAL-3 -1NORMALNORMALNORMALNORMALNORMALNORMAL0-20. 10490. 66690. 34092. 03070. 00305.53810. 14120. 85181.19803. 79900. 26019. 6190-3 0 +10.05540. 3337-0. 55480. 53050. 1042-2. 5508+20. 13430. 83831. 02143. 36680.23515. 0045+30. 21321. 34292. 59766. 20310. 366012. 55980. 29211. 84754. 17389. 03940. 496920. 11510.37102. 35215. 750011. 87570. 627827. 67040. 44992. 85677. 326214. 71200. 758735. 2257-3 0 +10. 04890. 1763-1. 57640. 54690. 1260-4. 8129+20. 13530. 74570. 86532. 77550.21554. 3704+30. 22171.31513. 30705. 00410. 305013. 55370. 30811.88455. 74877. 23270. 394522. 73700. 39452. 45398. 19049. 46130. 484031. 92030. 48093. 023310. 632111. 68990. 573541. 1036-3 0 +1 +20. 13481. 08823. 09604. 73940.22109. 0227+30. 20591. 76805. 37579. 33050. 308028. 14410. 27702. 44787. 655413. 92160. 395047. 26550. 34813. 12769. 935118. 51270. 482066. 38690. 41923. 807412. 214823. 10380. 569085. 5083-3 0 +1 +20. 09990. 81681. 30214. 24770. 25568. 3001+30. 17231.65614. 30789.44240.335227. 65750. 24472. 49547. 313514. 63710. 414847. 01490. 31713. 334710. 319219. 83180. 494466. 37230. 38954. 174013. 324925. 02650. 574085. 7297G7MAP UNIT GTPRAI-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0.0047-0. 3944-2. 5368-1. 06890. 0127-14. 3437MAP UNIT QTPAM-2 -1POTASIUMURANIUMTHORIUMU/KU/THTH/KDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMALMAP UNIT QTPAI-2 -1POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0. 11320. 1365-3. 4709-2. 59130. 0889-30. 7255-0.01150.6610-0. 73901.87450. 1642-11. 4365-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0.0992-0. 4936-3. 3934-1.4538-0. 1900-5.4095MAP UNIT GTTM-2 -10. 01040. 1959-0. 97311.72430. 00614. 93850. 12000.88541.44724. 90240. 202215. 2865-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0.1953-0. 2971-2.3451-0. 2863-0.05113.3110MAP UNIT GTTI-2 -1-0. 04160. 2050-0. 66991. 98680. 10549. 20760.11210. 70711.00534. 25990.261915.1042MAP UNIT GTPEM-2 -1POTASIUMURANIUMTHORIUMU/KU/THTH/KDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMAL0-20. 05330. 2900-0. 14542. 36660. 1202-0. 6034-10. 11130. 97442. 24605. 80210. 227713. 13690. 16931.65884. 63749. 23760. 335226. 87720.22732. 34327. 028812. 67310. 442740. 6175+20. 28533. 02769. 420216. 10860. 550254. 3578+30. 34333. 712011.811619. 54410. 657768. 0981-3 0-0.04350. 0696-0. 3418-2. 47050. 0888-6. 2125+10. 06110. 69001.77561. 00260. 16444. 2393+20. 16571. 31043. 89304. 47570. 240014. 6911+30. 27031.93086. 01047. 94880.315625. 14290. 37492. 55128. 127811.42190. 391235.59470. 47953. 171610. 245214. 89500. 466846. 04650. 58413. 792012. 362618. 36810.542456. 4983-3 0 +1 +20. 09021. 18551.99296. 34030. 23957. 8525+30. 19191.71004. 724810. 80610. 314827. 14150. 29362. 23457. 456715.27190. 390146. 43050. 39532. 759010.188619. 73770. 465465. 71950. 49703. 283512. 920524. 20350. 540785.008500. 22961. 57493. 86758.08050. 398325. 6345+10. 33922. 26446. 287811.25860. 594435. 9825+20. 44882. 95398. 708114.43670. 790546. 3305+30. 55843. 643411. 128417. 61480. 986656. 678500. 26581.20922. 68056. 53300. 418421.0008+10. 41951.71134. 35578. 80610. 574926. 8974+20. 57322. 21346. 030911. 07920. 731432. 7940+30. 72692. 71557. 706113. 35230. 887938. 6906-3 0-0. 0758-0. 0407-2. 0256-0. 3337-0.0208-8.0182+10.01190. 46410.00703. 06920. 10755. 3986+20. 09960. 96892. 03966. 47210.235818.8154+30. 18731.47374. 07229. 87500. 364132. 23220. 27501. 97856. 104813. 27790. 492445. 64900. 36272. 48338. 137416. 68080. 620759. 06580. 45042.988110. 170020. 08370. 749072. 4826G)Q~|MAP UNIT GTPEIPOTASIUMURANIUMTHORIUMU/KU/THTH/KDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMAL-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0. 1366-0.2247-2. 5103-2.2207-0. 0719-6. 0485MAP UNIT GTWM-2 -1-0. 02680. 3396-0. 58761. 72480. 09475. 37950. 08300. 90391. 33515. 67030. 261316. 8075-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL0. 02650. 2659-0. 70752. 4570-0. 11680. 0994MAP UNIT OTWI-2 -10.05540. 48160. 04804. 37670. 12536. 21020. 08430. 69730. 80356. 29640. 367412. 3210-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0.25010. 1161-1. 14251.2245-0. 0892-3. 3476MAP UNIT QTPPS-2 -1-0. 12000. 4868-0. 02944. 18040. 14185.37810. 01010. 85751. 08377. 13630. 372814. 1038-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL-0.08410. 2101-0. 1405-0. 5416-0. 00750. 3200MAP UNIT TPMU-2 -10. 00710. 73371. 53503. 15600. 121911. 19450. 09831.25733. 21056. 85360. 251322. 0690MAP UNIT TMHPOTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDIST0.05760. 39560. 67911.71850.052812. 3181-20. 08340.82001.86785. 06610. 172019. 2427-10. 10921. 24443. 05658. 41370. 291226. 167300. 13501.66884. 245211.76130. 410433. 0919+10. 16082.09325. 433915. 10890. 529640. 0165+20. 18662. 51766. 622618. 45650. 648846. 9411+30.21242. 94207.811321. 80410. 768053. 8657-3-0. 0161-0. 0442-2. 09470. 4225-0. 0588-4. 0683-20. 03810. 3771-0. 35232. 93230. 08446.3415-10. 09230. 79841.39015.44210. 227616. 751300. 14651.21973. 13257. 95190. 370827. 1611+10. 20071. 64104. 874910. 46170.514037. 5709+20. 25492. 06236.617312.97150. 657247. 9807+30. 30912. 48368. 359715.48130. 800458.390500. 19281. 46823. 25789. 61580. 427928. 2355+10. 30262. 03255. 180513. 56130. 594539. 6635+20. 41242. 59687. 103217. 50680.761151. 0915+30. 52223.16119. 025921. 45230. 927762. 519500. 11320. 91301. 55908. 21610. 609518. 4318+10. 14211. 12872. 314510. 13580. 851624. 5426+20. 17101. 34443. 070012.05551. 093730. 6534+30. 19991.56013. 825513.97521. 335836. 764200. 14021.22822. 196810. 09220. 603822. 8295+10. 27031. 59893. 309913. 04810. 834831. 5552+20. 40041. 96964. 423016. 00401. 065840. 2809+30. 53052. 34035. 536118. 95991. 296849. 006600. 18951. 78094. 886010. 55120. 380732. 9435+10. 28072. 30456. 561514. 24880. 510143. 8180+20. 37192. 82818. 237017. 94640. 639554. 6925+30.46313.35179. 912521. 64400. 768965. 5670-3NORMALNORMALNORMALNORMALNORMALNORMAL0MAP UNIT TMMPOTASIUMURANIUMTHORIUMU/KU/THTH/KDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMALDIST NORMALMAP UNIT TOSPOTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDIST-20. 06880. 88382. 22434. 45490. 168616. 5091-10. 10671.25533. 16647. 38960. 288223. 355100. 14461.62684. 108510. 32430. 407830.2011+10. 18251. 99835. 050613. 25900. 527437. 0471+20. 22042. 36985. 992716. 19370. 647043. 8931+30. 25832. 74136. 934819. 12840. 766650. 7391-3POTASIUMURANIUMTHORIUMU/KU/THTH/KDISTDISTDISTDISTDISTDISTNORMALNORMALNORMALNORMALNORMALNORMAL0. 01860. 20490. 8324-0. 04410. 03517. 4142MAP UNIT TEO-2 -10. 06510. 71482. 22263. 91360. 141717. 50010.11161.22473. 61287. 87130. 248327. 5860-30.02000. 3795-0. 64982.0504-0. 0228-0. 7793-20. 05830.79150. 95195. 28820. 126411.8785+1-10. 09661. 20352. 55368. 52600. 275624. 536300. 13491.61554. 155311.76380.424837. 19410. 17322. 02755. 757015. 00160. 574049. 85190.21152. 43957. 358718. 23940. 723262. 5097+30. 24982.85158. 960421. 47720. 872475. 1675-3NORMALNORMALNORMALNORMALNORMALNORMAL0. 03090. 51231. 28221.52020. 04909. 663100. 15811.73465. 003011.82900. 354937. 6719+10. 20462. 24456. 393215. 78670.461547. 7578+20.25112. 75447. 783419. 74440.568157. 8437+30. 29763. 26439. 173623.70210. 674767. 9296G7 wbLINE BASED MEAN CONCENTRATIONSAND RATIOS PER ROCK TYPEMAP UNIT GAL700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.250 0. 152 0. 182 0. 187 0. 150 0.236 0.276 0.364 0.285 0.347 0.423 0.299 0. 143 0.000 0.000URANIUM 2.357 1.646 1.422 1.646 1.375 1.456 1.670 1.940 2.008 2.345 2.758 2.258 1.536 0.000 0.000THORIUM 7.073 4.815 3.875 5.064 3.333 3.965 4. 168 5. 187 5. 591 7.334 6.616 5.800 5.213 0.000 0.000U/K 11.120 11.671 8.989 9.108 9.366 7.646 6.722 5.459 7.574 7.812 7.495 9.531 10.542 0.000 0.000U/TH 0.340 0.337 0.347 0.312 0.421 0.360 0.418 0.363 0.333 0.316 0.429 0.385 0.291 0.000 0.000TH/K 31.989 35. 109 27.413 29. 532 25. 956 23.057 18. 171 14. 514 20.962 25. 485 17.901 26. 686 38.823 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0.378 0.286 0.329 0.307 0. 198 0.364 0.000URANIUM 2.075 1.760 1.600 1.580 1.470 1.605 0.000THORIUM 6. 855 6. 244 5. 530 5. 131 5. 057 5. 078 0. 000U/K 5.805 6.036 6.245 6.315 8.207 4.754 0.000U/TH 0.304 0.251 0.296 0.303 0.278 0.295 0.000TH/K 19.351 23.925 21.408 23.348 28.464 15.378 0.000MAP UNIT GS700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 141 0. 000 0. 000 0. 000URANIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 1. 185 0. 000 0. 000 0. 000THORIUM 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 1.583 0.000 0.000 0.000U/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 8.246 0.000 0.000 0.000U/TH 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.759 0.000 0.000 0.000TH/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 11.915 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 199 0. 000 0. 000 0. 000 0. 000 0. 000URANIUM 0. 000 0. 929 0. 000 0. 000 0. 000 0. 000 0. 000THORIUM 0.000 2.915 0.000 0.000 0.000 0.000 0.000U/K 0.000 4. 593 0.000 0.000 0.000 0.000 0.000U/TH 0.000 0.341 0.000 0.000 0.000 0.000 0.000TH/K 0.000 14.750 0.000 0.000 0.000 0.000 0.000G8 wbMAP UNIT OHM700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.207 0. 189 0.229 0.221 0. 195 0. 194 0.202 0.219 0.221 0.213 0.238 0. 218 0.000 0.000 0.000URANIUM 1.153 1.419 1.405 1.383 1.118 1.067 1.401 1.642 1.161 1.619 0.976 1.144 0.000 0.000 0.000THORIUM 2.229 2. 504 3.436 2.626 2. 517 2. 306 3.050 2. 540 2. 977 2. 266 2. 196 2. 148 0. 000 0.000 0. 000U/K 5.118 6.940 6.523 7.309 6.796 5.795 7.620 7.045 5.833 6.565 4.959 5.110 0.000 0.000 0.000U/TH 0.351 0.293 0.349 0.291 0.368 0.321 0.381 0.427 0.339 0.353 0.416 0.443 0.000 0.000 0.000TH/K 11.066 13.283 15.759 12.292 14.266 12.163 15.423 10.249 14.232 10.442 9.661 10.415 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 236 0. 204URANIUM 0.000 0.000 0.000 0.000 0.000 1.830 1.044THORIUM 0.000 0.000 0.000 0.000 0.000 4.845 2.005U/K 0.000 0.000 0.000 0.000 0.000 7.563 4.619U/TH 0.000 0.000 0.000 0.000 0.000 0.336 0.442TH/K 0.000 0.000 0.000 0.000 0.000 20.693 10.238------------------------------------------------------------------------------------------------------------------------------------MAP UNIT GHI700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.256 0. 164 0.321 0.000 0.000 0.000 0.318 0.000 0. 000 0.000 0.234 0.000 0.000 0.000 0. 000URANIUM 0.908 0.816 1.383 0.000 0.000 0.000 1.629 0.000 0.000 0.000 1.537 0.000 0.000 0.000 0.000THORIUM 4.396 2.375 4.046 0.000 0.000 0.000 5.068 0.000 0.000 0.000 5.961 0.000 0.000 0.000 0.000U/K 3.501 5.352 4.682 0.000 0.000 0.000 5.116 0.000 0.000 0.000 5.720 0.000 0.000 0.000 0.000U/TH 0.212 0.350 0.336 0.000 0.000 0.000 0.321 0.000 0.000 0.000 0.254 0.000 0.000 0.000 0.000TH/K 17.733 15. 126 13.297 0. 000 0.000 0. 000 16. 023 0.000 0. 000 0.000 22. 863 0. 000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0.000 0. 000 0.000 0. 000 0. 000 0.000 0. 153URANIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000THORIUM 0.000 0.000 0.000 0.000 0.000 0.000 1. 141U/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/TH 0.000 0.000 0.000 0.000 0.000 0.000 0.000TH/K 0.000 0.000 0.000 0.000 0.000 0.000 7.693wbMAP UNIT GTSB700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0. 000 0. 000 0. 224 0. 171 0. 000 0. 135 0. 000 0. 284 0. 000 0. 194 0. 329 0. 000 0. 000 0. 000 0. 000URANIUM 0.000 0.000 1.061 2.089 0.000 1.766 0.000 2.476 0.000 1.945 0.967 0.000 0.000 0.000 0.000THORIUM 0.000 0.000 2.726 6.635 0.000 7. 125 0.000 5.929 0.000 4.412 2.773 0.000 0.000 0.000 0.000U/K 0.000 0.000 5.006 13. 129 0.000 12.385 0.000 10.916 0.000 9.295 3.079 0.000 0.000 0.000 0.000U/TH 0.000 0.000 0.389 0.311 0.000 0.241 0.000 0.376 0.000 0.257 0.371 0.000 0.000 0.000 0.000TH/K 0.000 0.000 12.601 41.448 0.000 55.413 0.000 20.189 0.000 23.118 8.470 0.000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000URANIUM 0.000 0.000 0.000 0.000 0.000 0.000 0.000THORIUM 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/TH 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000TH/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000-----------------------------------------------------------------------------------------------------------MAP UNIT GTPRAM700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0. 136 0. 000 0. 256 0. 000 0. 000 0. 163 0. 000 0. 000 0. 000 0. 000 0. 000 0. 208 0. 000 0. 000 0. 000URANIUM 1.573 0.000 0.000 3.303 0.000 2.226 0.000 0.000 0.000 0.000 0.000 1.850 0.000 0.000 0.000THORIUM 4.246 0.000 2.206 10.880 0.000 7.448 0.000 0.000 0.000 0.000 0.000 5.087 0.000 0.000 0.000U/K 10.422 0.000 0.000 0.000 0.000 18.962 0.000 0.000 0.000 0.000 0.000 8.859 0.000 0.000 0.000U/TH 0.339 0.000 0.000 0.312 0.000 0.237 0.000 0.000 0.000 0.000 0.000 0.319 0.000 0.000 0.000TH/K 30.647 0. 000 8.628 0.000 0.000 89.394 0.000 0.000 0.000 0.000 0.000 25.229 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 140 0. 000URANIUM 0. 000 0. 000 0. 000 0. 000 0. 000 1. 140 0. 000THORIUM 0.000 0.000 0.000 0.000 0.000 2.717 0.000U/K 0.000 0.000 0.000 0.000 0.000 7.655 0.000U/TH 0.000 0.000 0.000 0.000 0.000 0.367 0.000TH/K 0.000 0.000 0.000 0.000 0.000 22. 174 0.000-------------------------------------------------------------------------------------------------------IG10wbMAP UNIT GTPRAI700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.000 0. 194 0.216 0. 140 0. 145 0. 127 0.244 0. 154 0.000 0. 137 0.000 0.000 0.000 0.000 0.000URANIUM 0.000 1.083 2.130 1.387 1.086 1.097 0.000 1.509 0.000 2.023 0.000 0.000 0.000 0.000 0.000THORIUM 0.000 3.054 7.449 3.609 5.397 3.610 1.747 4.011 0.000 6.036 0.000 0.000 0.000 0.000 0.000U/K 0.000 5.663 10.373 6.841 7.551 11.115 0.000 9.766 0.000 9.906 0.000 0.000 0.000 0.000 0.000U/TH 0.000 0.336 0.295 0.323 0.200 0.325 0.000 0.433 0.000 0.331 0.000 0.000 0.000 0.000 0.000TH/K 0.000 16.736 37.075 22.740 37.852 28.494 7.265 28.370 0.000 30.358 0.000 0.000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 128URANIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000THORIUM 0.000 0.000 0.000 0.000 0.000 0.000 2.047U/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/TH 0.000 0.000 0.000 0.000 0.000 0.000 0.000TH/K 0.000 0.000 0.000 0.000 0.000 0.000 16.928MAP UNIT GTPAM700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.211 0.258 0.318 0.236 0.219 0.245 0.224 0.300 0.307 0.384 0.276 0.366 0.000 0.000 0.000URANIUM 1.989 2.205 2.761 1.880 1.924 1.867 2.029 2.117 1.962 1.601 1.543 1.717 0.000 0.000 0.000THORIUM 6.542 7.420 9.000 6.706 6.807 6.167 5.681 5.441 6.016 5.087 4.906 4.994 0.000 0.000 0.000U/K 10.108 8.937 9.711 8.619 9.497 8.546 9.719 7.444 6.717 4.453 6.099 4.894 0.000 0.000 0.000U/TH 0.297 0.296 0.312 0.270 0.274 0.307 0.364 0.336 0.321 0.312 0.322 0.329 0.000 0.000 0.000TH/K 33.220 30.343 31.395 31.826 34.443 27.915 26.977 21.229 20.927 14.482 19. 129 15. 134 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0.000 0.000 0.000 0.000 0.000 0.252 0.252URANIUM 0.000 0.000 0.000 0.000 0.000 2.070 1.449THORIUM 0.000 0.000 0.000 0.000 0.000 6.538 4.225U/K 0.000 0.000 0.000 0.000 0.000 9. 170 6. 178U/TH 0.000 0.000 0.000 0.000 0.000 0.315 0.342TH/K 0.000 0.000 0.000 0.000 0.000 28.558 18.268G11 wbMAP UNIT GTPAI700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.000 0.146 0.000 0.113 0.000 0.193 0.275 0.000 0.162 0.000 0.000 0.478 0.000 0.000 0.000URANIUM 0.000 0.000 0.000 1.709 0.000 2.210 0.000 0.000 1.721 0.000 0.000 2.289 0.000 0.000 0.000THORIUM 0.000 1. 606 0. 000 5. 554 0.000 8.967 1.641 0.000 4. 169 0.000 0. 000 5.798 0.000 0. 000 0.000U/K 0.000 0.000 0.000 11.513 0.000 13.340 0.000 0.000 13.251 0.000 0.000 4.796 0.000 0.000 0.000U/TH 0.000 0.000 0.000 0.316 0.000 0.248 0.000 0.000 0.244 0.000 0.000 0.397 0.000 0.000 0.000TH/K 0.000 11.209 0.000 50.518 0.000 54.406 5.976 0.000 23.977 0.000 0.000 12.182 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0.000 0.000 0.000 0.000 0.000 0. 156 0. 123URANIUM 0.000 0.000 0.000 0.000 0.000 1.465 1. 170THORIUM 0.000 0.000 0.000 0.000 0.000 4.049 2.486U/K 0.000 0.000 0.000 0.000 0.000 10.599 10.649U/TH 0.000 0.000 0.000 0.000 0.000 0.333 0.433TH/K 0.000 0.000 0.000 0.000 0.000 27.563 25.534MAP UNIT GTTM700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.000 0.000 0. 127 0.089 0. 122 0.099 0.331 0. 161 0. 165 0.291 0.000 0.000 0.000 0.000 0.000URANIUM 0.000 0.000 0.996 0.851 1.127 1.048 2.258 1.441 1.396 1.910 0.000 0.000 0.000 0.000 0.000THORIUM 0. 000 0. 000 2. 497 2. 176 2. 824 3. 189 6. 140 2. 525 5. 367 6. 070 0. 000 0. 000 0. 000 0. 000 0. 000U/K 0.000 0.000 8.233 0.000 9.678 0.000 8.777 10.306 9.069 6.798 0.000 0.000 0.000 0.000 0.000U/TH 0.000 0.000 0.408 0.378 0.396 0.356 0.382 0.614 0.263 0.309 0.000 0.000 0.000 0.000 0.000TH/K 0.000 0.000 22.402 27. 148 24. 507 39.233 24.961 25.388 36. 158 21. 572 0.000 0.000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 229 0. 000URANIUM 0.000 0.000 0.000 0.000 0.000 1.516 0.000THORIUM 0.000 0.000 0.000 0.000 0.000 2.971 0.000U/K 0.000 0.000 0.000 0.000 0.000 8.434 0.000U/TH 0.000 0.000 0.000 0.000 0.000 0.450 0.000TH/K 0.000 0.000 0.000 0.000 0.000 25.989 0.000G12 wbMAP UNIT OTTI700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.121 0.116 0.112 0.000 0.089 0.117 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000URANIUM 0.923 0.903 0.925 0.975 1. 129 1. 502 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000THORIUM 1.968 1.897 2.049 2.208 2.793 3.601 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/K 8.067 8.312 7.641 0.000 0.000 11.555 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/TH 0.435 0.381 0.477 0.406 0.361 0.403 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000TH/K 25.210 29.673 23.013 0.000 20.087 32. 179 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0.000 0.000 0.000 0.000 0.000 0.390 0.000URANIUM 0.000 0.000 0.000 0.000 0.000 1.658 0.000THORIUM 0.000 0.000 0.000 0.000 0.000 4. 175 0.000U/K 0.000 0.000 0.000 0.000 0.000 5. 576 0.000U/TH 0.000 0.000 0.000 0.000 0.000 0.415 0.000TH/K 0.000 0.000 0.000 0.000 0.000 17.651 0.000MAP UNIT OTPEM700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0. 145 0. 155 0. 159 0.209 0. 125 0. 138 0. 140 0.257 0.000 0.000 0.000 0.000 0.000 0.000 0.000URANIUM 1.604 1.113 1.292 1.841 1.407 1.492 1.582 1.890 0.000 0.000 0.000 0.000 0.000 0.000 0.000THORIUM 4.524 3.213 3.749 4.317 3.961 4.217 4.402 4.632 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/K 15.694 9.649 7.747 9.939 13.287 9.926 11.346 8.277 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/TH 0.386 0.373 0.359 0.281 0.358 0.357 0.378 0.424 0.000 0.000 0.000 0.000 0.000 0.000 0.000TH/K 57. 561 40.250 28.324 34.394 46. 527 37.454 40.605 20.460 0.000 0. 000 0.000 0.000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0.000 0.000 0.000 0.090 0. 113 0.000 0.000URANIUM 0.000 0.000 0.000 0.843 1.588 0.000 0.000THORIUM 0.000 0.000 0.000 1.580 4.804 0.000 0.000U/K 0.000 0.000 0.000 8.996 13.555 0.000 0.000U/TH 0.000 0.000 0.000 0. 539 0.281 0.000 0.000TH/K 0.000 0.000 0.000 25.670 47.811 0.000 0.000IG13wbMAP UNIT GTPEI700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.000 0.100 0.104 0.088 0.106 0.084 0.122 0.000 0.112 0.190 0.000 0.000 0.000 0.000 0.000URANIUM 1.558 1.100 1.443 0.780 1.023 0.976 1.649 0.000 0.824 0.927 0.000 0.000 0.000 0.000 0.000THORIUM 4.049 3.069 3.865 1.528 2.128 1.184 4.493 0.000 1.890 2.586 0.000 0.000 0.000 0.000 0.000U/K 0.000 10.555 8.123 8.557 9.015 0.000 9.192 0.000 0.000 3.701 0.000 0.000 0.000 0.000 0.000U/TH 0. 349 0. 372 0. 402 0. 516 0. 472 0. 770 0. 339 0. 000 0. 482 0. 369 0. 000 0. 000 0. 000 0. 000 0. 000TH/K 0.000 33.246 19.284 14.873 26.620 12. 362 30.830 0.000 16.884 16.461 0.000 0.000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 156 0. 100 0. 000URANIUM 0.000 0.000 0.000 0.000 1.225 0.951 0.000THORIUM 0. 000 0. 000 0. 000 0. 000 4. 735 2. 130 0. 000U/K 0.000 0.000 0.000 0.000 7.988 9. 158 0.000U/TH 0.000 0.000 0.000 0.000 0.251 0.478 0.000TH/K 0.000 0.000 0.000 0.000 32.710 21.084 0.000-------------------------------------------------------------------------------------------------MAP UNIT GTWM700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.088 0.088 0.000 0.136 0.000 0.129 0.000 0.186 0.119 0.232 0.000 0.000 0.000 0.000 0.000URANIUM 0.000 0.849 0.000 1.155 1.253 1.184 1.563 1.521 1.566 1.806 0.000 0.000 0.000 0.000 0.000THORIUM 0.803 1.195 0.000 2.486 2.860 2.742 2.145 2.867 4.017 4.511 0.000 0.000 0.000 0.000 0.000U/K 0.000 0.000 0.000 8.116 0.000 11.076 0.000 10.307 11.416 9.809 0.000 0.000 0.000 0.000 0.000U/TH 0.000 0.879 0.000 0.489 0. 450 0.440 0.689 0. 527 0.377 0.373 0.000 0. 000 0.000 0.000 0.000TH/K 0.000 8.987 0.000 26.527 0.000 32.709 0.000 28.762 31.213 30.980 0.000 0.000 0.000 0.000 0.0001180 1190 1200 1210 1220 1230 1240POTASIUM 0.000 0.000 0.000 0.103 0.215 0.142 0.000URANIUM 0.000 0.000 0.000 0.845 1.446 1.270 0.000THORIUM 0. 000 0. 000 0. 000 2. 096 3. 764 2. 567 0. 000U/K 0.000 0.000 0.000 9.538 9.068 9.293 0.000U/TH 0.000 0.000 0.000 0.399 0.342 0. 535 0.000TH/K 0.000 0.000 0.000 23.035 27.515 19.656 0.000G14 wbMAP UNIT GTWIPOTASIUMURANIUMTHORIUMU/KU/THTH/KPOTASIUMURANIUMTHORIUMU/KU/THTH/K7100.0000. 8891.6690. 0000. 6090. 00011900. 0000.0000.0000. 0000.0000.0007200.0000. 7500. 8700. 0000. 9420. 00012000.000" 0.0000.0000. 0000. 0000. 0007300. 0000. 0000. 0000. 0000. 0000. 00012100. 0950. 8071. 2657. 6300. 69114. 0797400.0000. 0000.0000. 0000.0000.00012200. 1381. 0972. 9057. 8600. 37923. 2397500. 0901. 1741. 9619. 5370. 56010. 31812300. 0000. 0000. 0000. 0000. 0000. 0007600. 0001. 1082. 3170. 0000. 5020. 0007700. 0000. 0000. 0000. 0000. 0000. 0007800. 0000. 0000. 0000. 0000. 0000. 0007900. 0000. 0000. 0000. 0000.0000. 0008000. 0000.0000. 0000. 0000. 0000. 0008100. 0000. 0000. 0000. 0000. 0000. 00011500. 0000. 0000.0000.0000. 0000. 00012400. 0000. 0000. 0000. 0000. 0000. 000MAP UNIT QTPPSPOTASIUMURANIUMTHORIUMU/KU/THTH/KPOTASIUMURANIUMTHORIUMU/KU/THTH/K0.1171. 0221. 4689. 3550. 73619. 28311800. 0931. 1671. 80210. 5300. 65217. 6067000. 1000.8201. 2419. 4840.65916. 49711800.0000.0000.0000.0000.0000.00011600. 0000. 0000.0000. 0000.0000. 00011700.0000.0000. 0000. 0000. 0000. 000700 7100. 1071. 0691. 59410. 0490. 73024. 55111900. 1571. 1092. 0069. 1710. 58423. 6497600. 1431. 6533. 07711. 8090. 59820. 1437200.1451.1691. 9239. 2850. 65019. 90912000. 2191. 1102. 2918. 2640. 48721. 2077700. 1341. 5192.60711. 1160. 66127. 1917300. 1131. 1642. 00210. 3480.62121.27412100. 1181. 2382. 8717. 7760.45421. 5757800.1131. 3092. 65710. 9660. 53327. 4717400.1021.2752. 29510. 6000. 57522. 71412200. 1341.4525. 37910. 6200. 27440. 5777900. 1141. 1842. 0899. 8600. 60521. 0857500. 1111. 1372. 1329. 9700. 58824. 67712300.0000. 0000. 0000. 0000. 0000. 0008000. 1151. 3122. 84211. 8590. 47525. 1868100. 1331. 8613. 99215. 0620. 52237. 06411500.0000.0000.0000.0000.0000. 00011600. 0000. 0000. 0000. 0000. 0000. 00011700. 0000. 0000. 0000.0000.0000. 00012400. 0000.0000.0000. 0000. 0000. 000G15 wbMAP UNIT TPMU700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.000 0.104 0.124 0.179 0.128 0.158 0.164 0.169 0.196 0.224 0.208 0.216 0.157 0.136 0.159URANIUM 0.000 1.125 1.267 1.398 1.405 1.582 1.871 1.909 1.647 1.737 2.179 2.084 1.543 1.567 1.937THORIUM 0.000 1.684 3.639 3.731 3.729 4.338 4.734 4.514 5.208 5.268 5.597 5.777 4.750 5.030 5.258U/K 0.000 0.000 10.017 9.719 11.378 10.992 11.592 11.054 9.846 9.894 10.829 11.010 9.812 11.452 12.196U/TH 0.000 0.701 0.345 0.414 0.415 0.384 0.408 0.452 0.335 0.341 0.397 0.374 0.332 0.321 0.388TH/K 0.000 17.246 30.074 32.643 34.059 33.967 34. 177 33.212 33.390 31.610 30.652 32.643 33.496 41.741 37.6221180 1190 1200 1210 1220 1230 1240POTASIUM 0. 197 0.233 0. 159 0.208 0. 131 0.000 0.000URANIUM 1.758 1.486 1.309 1.359 1.310 0.000 0.000THORIUM 5.057 4.212 3.817 3.797 4.330 0.000 0.000U/K 10.491 8.270 8.421 7. 139 9.979 0.000 0.000U/TH 0.379 0.394 0.361 0.308 0.293 0.000 0.000TH/K 33.685 27.885 28.930 26.804 35.387 0.000 0.000---------------------------------------------------------------------------------------------------MAP UNIT TMH700 710 720 730 740 750 760 770 780 790 800 810 1150 1160 1170POTASIUM 0.136 0.125 0.134 0.133 0.139 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.110 0.147 0.117URANIUM 1.734 1.803 1.668 1.763 1.427 1.353 0.000 0.000 0.000 0.000 0.000 0.000 1.674 1.643 1.345THORIUM 4. 399 4. 103 3.961 4. 727 4. 092 3. 892 0. 000 0. 000 0. 000 0. 000 0.000 0. 000 4. 224 4. 597 3. 414U/K 13.360 13.388 11.918 11.446 9.422 0.000 0.000 0.000 0.000 0.000 0.000 0.000 11.766 10.815 10.830U/TH 0.406 0.456 0.432 0.389 0.355 0.355 0.000 0.000 0.000 0.000 0.000 0.000 0.401 0.378 0.421TH/K 33.038 33. 164 29.216 35. 149 32.788 0.000 0.000 0.000 0.000 0.000 0.000 0.000 36.385 33.666 32. 5021180 1190 1200 1210 1220 1230 1240POTASIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000URANIUM 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000 0. 000THORIUM 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000U/TH 0.000 0.000 0.000 0.000 0.000 0.000 0.000TH/K 0.000 0.000 0.000 0.000 0.000 0.000 0.000G16wbMAP UNIT TMMPOTASIUMURANIUMTHORIUMU/KU/THTH/KPOTASIUMURANIUMTHORIUMU/KU/THTH/K7100.1291. 6543. 50512. 0260.49728. 99711900. 0000. 0000. 0000. 0000. 0000. 0007200. 1441. 5253. 89011. 5490. 42335. 89712000.0000.0000.0000.0000.0000.0007300. 1371. 5884. 37511. 1210. 40536. 36112100. 0000. 0000. 0000. 0000. 0000. 0007400. 1361.5774. 93210. 9580. 33238. 88912200. 0000. 0000. 0000. 0000. 0000. 0007500. 0000. 0000. 0000. 0000.0000. 00012300. 0000. 0000. 0000. 0000. 0000. 0007600. 0000. 0000. 0000. 0000. 0000. 0007700. 0000. 0000. 0000. 0000. 0000. 0007800. 0000. 0000. 0000. 0000. 0000. 0007900. 0000. 0000. 0000. 0000. 0000. 0008000.0000.0000.0000.0000.0000. 0008100. 0000. 0000. 0000. 0000. 0000. 00011500.1271. 7185. 27312.5650. 34147. 68812400. 0000. 0000. 0000. 0000. 0000.000MAP UNIT TOS750 760POTASIUMURANIUMTHORIUMU/KU/THTH/K0.0000.0000.0000.0000.0000.0001180POTASIUMURANIUMTHORIUMU/KU/THTH/K0. 0000. 0000. 0000. 0000. 0000. 0000.0000.0000.0000.0000.0000.00011900. 0000. 0000. 0000. 0000. 0000. 0000.0000.0000.0000.0000.0000.00012000.0000.0000.0000.0000.0000.0000.0000.0000.0000.0000.0000.00012100.0000. 0000. 0000.0000. 0000. 0000.0000. 0000. 0000. 0000. 0000. 00012200. 0000. 0000. 0000. 0000. 0000. 0000. 1411.7354. 40012. 1080.39531. 46712300. 0000. 0000. 0000. 0000. 0000. 0000. 1442. 0045. 32512. 2930. 38137. 5830. 1681.6994. 6788. 3630.38525. 7570.117 0.1211.400 1.5443. 829 3. 60711.507 10.9800. 363 0. 43531.801 31.51912400. 0000. 0000. 0000. 0000. 0000. 0007000. 1231. 6143. 68713. 1710. 46435. 41711800. 0000. 0000. 0000. 0000.0000.00011600. 1321.6805. 17413. 3370. 36045. 51711700. 1181. 7103. 29313. 7140. 53728. 630700 710 720 730 740 770 780 790 800 810 1150 11600. 1402. 1073. 81216. 3070. 59224. 15311700.1861. 7554. 2859. 2250.41624. 6370. 1311. 4273.9149.8050. 37032. 9770. 0000. 0000. 0000. 0000. 0000. 0000. 0000.0000.0000.0000. 0000. 000- ------G17 wbMAP UNIT TEDPOTASIUMURANIUMTHORIUMU/KU/THTH/KPOTASIUMURANIUMTHORIUMU/KU/THTH/K7000. 0000. 0000. 0000. 0000.0000.0007100.0000.0000. 0000. 0000.0000.00011900. 0000. 0000. 0000. 0000.0000. 0007600. 0000. 0000. 0000. 0000. 0000. 00011807200.0000.0000. 0000. 0000. 0000. 00012000. 0000. 0000.0000. 0000.0000.0007700. 1611.7785. 2989. 4570. 34035. 8107300. 0000. 0000. 0000. 0000. 0000. 00012100. 0000.0000.0000. 0000.0000.0007800. 1231. 2984. 3108. 5760. 31238. 6127400. 0000. 0000. 0000. 0000. 0000. 00012200. 0000. 0000. 0000. 0000. 0000. 0007900. 1811.4585. 3728. 7600. 28737. 6447500. 0000. 0000. 0000. 0000. 0000. 00012300. 0000. 0000. 0000. 0000. 0000. 0000. 0000.0000.0000.0000.0000.0008000. 1572. 0144. 64616. 2940. 43944. 1798100. 1772. 0305. 68813. 2570. 35938. 56911500. 1391. 6364. 65911.9660. 35935. 88611600. 0000. 0000. 0000. 0000. 0000. 00011700. 0000. 0000. 0000. 0000. 0000. 00012400. 0000. 0000. 0000. 0000. 0000. 000APPENDIX H - Pseudo Contour MapsCI l - 111 T Iflu*JicrL UrJ[p~: TE 1JflfIE J1IL 1I T JIf J .1..,, L~ UJ...lBI .JUt F. TWLl &T J.flLUWiJL IITEJflIJ c4u tz -"Uk ". r -- f3V% j.' i 'a r:' m3"+,; C NF {,,w':_ i', ?J.1'y "-OnntH1wbWAYCROSS++ +++++++++++++++ +++++++++++++++++++++ +++ ++++++ +++++++++++++++ +++++++++++++++++++++t")C')C)qtCV)NC'444C')CU(V NNNNC') CU~NNNNC') CUCNNCNNNNNCUN NnNNN NN NNNNNNCuCNCNN NN NN NNNNNNNr) rCUCUrd) CU CUC') CU CUrdUdCUCUCUN NUCrd rd rdCUCUrCUCCUUCCUUCNNUCNCNIri IdCurdrdNCCurdNICUICU1C,C,)C')C')C'NNNNNNUCUCUNrCCUCUdUrdrd rd rrd rdCrdCdCUrd CUdCU CCUCUCCUCUCNNCUNCNCNCNCN NCNNNNNNNCNCNNCNNCNNNNNNNNNNNCUCUNCNCNNN NNNrdrdNNNrCVCUCUCUN NNN (VCV) NCU NNrdC C')NN C'NCUCU CUCU CUCUCUC CUCUCU CUrd dCUCUCUNNCUCdCUCU CUCUNNNINNICUCUCUCUCUCUrdCUCUCUCUCUCUCUCUCUCUCUCUCUCUCUCdCUNIrdCUNiNIIVCUCUCUCUCUCCCUCCUNCNN N N rd(VrdCUCU CUNNNCUCUUCUCCUUUCCCUNCUCUrdCUrdCUrdCUCUCUrdCUCUCUCUCUCUCUCUCUCUCUrdCUCUCUCUCUCUCUCUCUrdCUC)CCUCuNCuCuNUCuCuCuCuCuNCUNNCuUCUCUCUCUCUNNN NNNN NNNNNrdrd N NN NN(VN (J CrrN rd rd rd rdt11r t1Nt N Mrd rdr dr N t11NNNt1NNN ~tNNNCUdUC CUCC')C) '00Q++++.4N O NNNNNNNNNN et NNNNNNNNN NN 1 NNN NNNNNC ') N NN ' NN M NNC ) NN n NNN ') NNN ) CN NN N N NNNN N N d dNN NN N N N NNN NNNN rd Nrdr dNrrNNNNNNNNNNNNNNNN NNN d d d r r CNN N NNN rd d rNN NNNN NNNNN NN at' NNNN NN N '' NN N N N N (NNN NNN C NN N NNNNNN NN CUrdrdCU NNN N N NN N NN NN NN NNN NNN N NCUdCUdCUdCUC M (' O CM Nit i et MMCn'C InI 4MM M n1" tvvmNN 0M00 It NNNNNN M rd MMNNN NNNNMMNMM M .0 nan4 CMt) t MM In n nMUCUN, CN CU CUCMCUd rdCV rNC M C'n -0 .0 M ) ) C) otd CU In'0In4 C) 4 CU C) C ) CMNN MN ('3C')C)4 ' In rd CNU ')f' U 'N 0 04 4t 4) C 'N M) (3 U M inN M MMN C NNN( MM .4« 0 nUC ' (' 'In MC') M C') ' CN N MM3M') C) CW 4) U) ) C) ' I" f 4 ) NM'M C' %4'CON 'M) (3 InC ' C') CM CMo' '-M «0 In W (NM'3 4N NNMMM eMM MM M.ot MM NN N he n a NM 4' M f * MmN NNN M ' InOD (')(') C' 4C') C')'M M CU mf I n tM0 Iot4 CUC C) 4 O '0ONrU rd rd (')C' 44 M ')(')In NIn4qt nnn4 (MMM of -0 f ) ( NNM'0 ) ) 'MNNNNN M UC 4 'C 0 4 In 00'0n4% C')C'Mot n 4 ' M CCNNN MM n I NNINNNNnM i4t4n r0 4 C')M'0 o 4 in 4 CM ) U CU 3 CU C) C M '0NN NN C) 4 4 COW .04' n4OC ] 4*4 () MUNCUC N N N N C UnnNN N I 4 In C') ' 0'OCOit4 NfOG CUU U NNNNN N NN N')CN N N NCotCINN N 4 C'0OO % CO NNNN NNN N N NM NN of C) M)O*"G'O N of N4Oh N « ««'4 CU N'N (' 4 4 ' ft C') C ) M O'DaOn C') '4 '4''«««« C «CU M') 44 C')n INN 0 44 COO(P CO M') .4 NNC '4' '44«««« '44« ««««'N M MM 4' M MM 0 0 ot %0 " et NN « « « « « «C M C' 4 a(' C')n 1 n 000'0 44 '0N O" 4 '4dW « «M')4 CUfC')M') n 0- (M3NCU MCN)C«««U««««««( N 't NN )n CO C NN Lt'3C3««««.+«SNNNM' CCU C')C'M C')C)t «0«CMI 0' CU NU C4''CVCVNUC CUMNNMotNM 0 «' 04 r) CU )N NN C«««rrNNNN nnNrd M NNNN N4CO 0«N nnN NN« «rdCUCUCd CU ('drd)CrUrCNN ') CUCUdUd U td0 d d i N00'4 CU C')N CUU «««««N N N N NNN N U N N N N NN rdCMUCUC CUC CU 4 I0I 00' C ('.N CUCU4'4 « « «rd d d r r r NNNNN NN NNN N NM **** N rd NNNN NN '« « «NN UUNCUUN NN NNNN NNN N N C')44"4n NN0 C U C NUCUNNNNN -NN NNNNNN NNN N M MM r NN «4+«NNNN 4NN NNNNNN NNN N MMMMNN «««« N NN N .CUUUC NNNNN NCUCCUCNUCU CUU UCCU C ) 4 rd 0'd '4C U'4'4'N NNNNNN NNNNNN C NNN N NNNNNNN '4 CU W4CU N N NCNUCUN4 NCUCUCUCU '4 CUCUrdCUCUCUCUCUd CUCUCUCUCU rd'rdCUCUCUCUd '4 4 '4'4'4 CU CUrd dCUCU '4'4 N '4N N N NNNNNNNN(VI NNN rd d r rdd N N ;4«4 NN NNC CCNU C C N NNNN CUCU UCUUUNN NNNNNCUUCU ' '4« C'«U UNU ''NN 4CUUCUNNCU CUCUCUUCUCUCUC CUCUNUN CUCUNUC rC '4 '4"MCU N rUCrC N UCU CU CU CVCUNNC U N N NCdCCC CUCUCUCUC n «UCC N NNN NNMM NNNNCUCUCU CUUNN MM N N NC NNNNr ) ' CU CUCUNNCNNNNNNNNNN1N NN MMMM N N N rdrdN N MM N NN NNotq Md r r rdrdrd d d r r NN MMM N N NN N M NN Nry NNMN NN NNNNNNN MM N NN N N IN rN NN rd NNenN NN NNNNNN MM N d rdNrd N N r dr dr dNN NNnn rd n N NN e NN dr dM dNrN r r N NN N .4 4 N N Nnn N NN M d d d d N rd rd MM N N Nrdr N «.4 N N '.NCU C NNU C CCNNNNNNNN N N NNNNNiCU 4« «.U.4 Nn N NNN MN NNNNNNNNunnNNN N NNNNNN «94* .4«NCC UU NNNUM)rU CU )CCUUd4rCNN N NNNNN NNNNNN')'C4' NNNNN M r rdrdrd d r r N N NN NNNNNNN ««« «MM NNN N NNNNNNNN N N NNNN N .«4 ««44NNMM N NNN d r rdrNNN 9 drdr d«« N « «N.« «M N NNNNNNN CU C ) C CU C ' C4 )««.) U N U « CCN N NNN NN N «.4«N NN N .. 'N N N N« « « « NNN NNN NNN « N " WINn CU CC (3 CCUUUU '19' '1r CUNCUUCUUC CCN N UCNNN U4C C CUCUC UC«' N N «4 CC CNNN UU «CUUCUU U CUCC UNCUUUCC« 'NN '+NNNNNNN « «4 ««.«4 «NMM M .4«NN « N N «NNNNNN CCCC«« UUUUUUU U C CUU CCMMC' '4 NN '4NN CNC.1 « «CUCUCU«CU4.4.4.4C« CUCUCU«'44CUCUCU NCU M MMN «'1 « ' M CU '4 N N NNN NC«)4U.CCUCUUCUU.CU.4«CUCCUC CU .4.4 CNNNNU«N N NN CU«UCCU CUU«U«.4« «UCCUUNCCU CUU M4N «C NNNN «N NCU C 44 '44« CUCUCU«CUC N N NN CUUU'4 '4 CU4'4r« N N N «NN NN N N N '4''44'+«CCUUU CCU CU«.4.4«««C U C U C U C U C U C U.44«4'44«4.4'44«4 4«CU CU)'4 N N N N N U « .4« Nn * NN NN NNNCNCNUCUCUCUCUCU.'9-4 '4.'..4'«.'4«4 ««' 4« 4 U CUC U N4NS N .NCUCUCUCUCUCUCU '4 «'4' '44 '4.(«.4«)194««« '4'4 CUCU ' CU4CU«14WNrd d NN '«4 « « « « « ««M « « « « N N N .«N NCN NCNC '4 ''44V44'4C.4'«' .4 4«CUCU '4NCN N '4'NNN NNCN '4 N'« 4 '4 4.4.4« 4 «««'1«.4««).4 .1«««'M4NUC«.CUC CUd''N''4N ««4 r444'«4 «.'4 «44 «««««« C'CU''4'.4 .44« « N'. 4 CCUUC4.CUNCUCU '4'4''44'44'4'1-'44'44'4'4 CU9'44 - 4«'4'.4 «'4« C « « «CU 4 CUCUCUC« .NCU CU «CU '4 «««« 4'4 «44 ««.44 «4' 4 CUUCUUCU«4'4««4'4««( «««.-'4 ««CU «CU «.NNNN . 4 « « 4 « «44 « .« 4.1 44"« 44 « 44 « « «NUC CUCU CU«« .1«CU . CU .44 4 '44 4 4 . 4' 44 4 /'.4 CU4 444 4 4 C)'4 4 CUCUCUCU «'«NU CU CU 4'4« 4 49CU 4 CU4. .444444444 4 «« 4 4 4 «'444 .4'94'«4 «('34 C'«U C «CUCU .4CU CUN CU.4CU4CU.4 CU .4 4 4 4 '4 « 4''4 «'444«4 4'4 "'4«'4 . 4 .4 4 4 4 «C')44 C'« CUCUCU U.4 4CUN CU CU4 9CU.4C.4 4 444'' 44, 4. 4444 « 4'4' 4'44' .44444 4 «. 44 «) U U «U U 94 .4CUC9UC-''''''4''' 4444444'N '' p ' 4 4' 44 W 4 4 4 , 4 ««'4 4 .CU+ CU CU CU '4'4'4'4'4,4 '4'+'4+'4'4'4'4+4 '4'4,4,4,4,4,4,4,4,4 '4,4,4,4,4 '4'4'4'4'4'4,4'4,4,4,4'4CUUUU ' 444444'' 444444444,,,,, 4444444 ',''',',,,CU+C+CU++U++++++++++++++++++++++++++++++++++++++++++++ '4''4'4''4 +++++++++++++,4'NN +unn ~+ICUC')C ') +CV) N +44. C+4f4 In 0+In 0+I1In'0 '+IIn In n C') +0 +4e +in f,%CD +Ch+C'C' +CU 4 +NN +N +C) +'44NC +t'7 +N' +'40 +O4+'4++'+N +CU +NU +CUC+NUCU+NUNU+CU++N+NN ++'4+'4+'4 +"f +'l,4 ,4 +'4,4,4,,4+4 '44 +++) +4+N m+4+ +CV)C) +NU1r) t('3+'N CU +N4, +'4,4 +'4,4,4 +-', +'4,4, +'.4,4 +++++N ++4.4.4+4.4.0 LE'"4'.4.'4'4OT 0. 4500Potassium Pseudo-Contour Map - Waycross QuadrangleEXPLANATION0.00001 0.02500.05002 0. 07500. 10003 0. 12500.15004 0. 17500.20005 0.22500. 25006 0. 27500. 30007 0. 32500. 35008 0. 37500. 40009 0.4250C7NCNrdCdrdrdNCr)CNNrdrdrdCdCUCdCUrdNNCUVALUE0. 00C0.0.0.07500. 10000.12500. 15000.17500. 20000. 22500. 25000.27500. 30000. 32500. 35000. 37500. 40000. 42500.4500PRINTCHARACTERiSCALE IN EQUIVALENT PERCENTH2 wbWAYCROSS+++++4. +.+ ++ ++ ++ ++ + ++.+ + +4+ +4+.++ +++.+.+ + + +.+ + +4++ ++ + +++ + + + +++ + ++ ++ ++ ++ + ++4.+ + + + + +40'0444*0ItI.I.I.I.(')ci'3'3C3(3IfM4(13('3IC'13InIn44.V) MCI3Cry('3('('3(V)('3C7C,('3M'('('(''('('3(134.4. ('4.4.t4.4.4.4.4.4.4.4.4.dV'('('3MM1'4.4.4.4.4.it4.4.4.4.('3('33('34.hitqt4tq'4.,a.d'. 4.4.'4.'d'4.'('3('3('3"h('('I'3t"4.4.4.It4'4.4tft4.it("'MMIMMMMM'('('('M'('('MM('3('3('3MMMMMMMM'MMI4.4.4.4.4.4.44.44.44.44.44.4.('3('(1("('('('("'("'('(e( CO)C7a.4.4.a4.4.R'V'4.t?et4. 4.4.d' 4.4.M M4. 4.4. 4.M M 4.M MMMM44.4.44.4.4. ('4.4. ('3(1(te '3(e)et('3(e)('3 (' 4(3Tof3('('3 '('3 (3 ('3('3('('3 ('3('3('("('3(13r Kqt'9-t 4(1i('(1(e('3(t'3I t'(1I(''3('3('3('3('3('3('3('('('('4.4.4. 4.4.4. 4.4.4. 4.4.4. ('34. ('3 ('3('3('34.4. 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C C 13('3N(V rd -+ C N('3 4 'T ') 4. 4. 1 1()1r) rdCU(14. 4.4..44..4. ".4 it t)C 4.t4. C1 C1 C13(C1 rd ''-4.4..4.. (3 4. (e)e3(3 '4.4.4.etIn 4.4.n 4.4..n0n 4n n 4. e4t .Innn t4'4.In~n 4Inn~n 4.'0n nn In 4.'0 In n In In4..t%0,4 4 .I In40 4.4. In .%0 netd n" %- 00to nn0 n .ot n'0%0'0In 4. U)I'0'ISn 4. 4.I nIn t qt.o 4 tit 4.it44tIn 4it '' VVMjt 9t4 t '4.44.44.4 4.4.44..4 4.$ 44.44.4 4.4.44. .4.4 4.4.44.44.4 4..4.44.4 4.4.4.4.4.4.4 4.4.4.4. 4. 4.4.4('S'li4. I.d'4.4.4.4i4.4'It4.%td'4.4 (C (C)C)('34.4. 4. ('34.4 4. 4.4. 44 4. 4m '4 .4.4 4. 4.4. 4. . 44.44. 4. 44.44.4. 4..4.4NNC CUCMN NNN NN NN NN rd rd rdN rd rd rdN "+- r 1 N NNN - NN NNNN NN NNNNNt1NNN NINN NN N NIN N NIN t CV N NI1 C1 N N CMC1ir N NNNmN("("N NNNNNINC N NNICU N NNCIC)V NN NNIc CV) NNN NNrd C dU CnnInInIn'0'0 0'0 '0'0 I'0'0 q0 1InInenma.'Q'4.m C',('344.44. 44.4. Ino4. 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(3 Cy('( ) CUCUC 1('3N ('3 P)(3 4d' '3 N CUCU C nCU ('3()3 i t C' (3 NN N C (N (' N ' ('3 ('3 CUCNN NNC '3(')(e1 CU'')(N1NN3NN enP)(c V) CU (' N N NN( (a('3 NN NCUC CN N'(3() cm' NNC UNNCU1CUC1C (3 ((, (C U rCU NNCUN(NN'3 (1'3CU CUCUCU dUCUr('NN NN3('' 1CUCoN NNrdNN NN N N m C)1UN N NNN N C C UCC CUNN N Nr r d drdr )) N NN N N N rd d d r NNN v4 CUCUCU d N CUC NNN f+ NNNNN N rd rd rCu " NNNNNN N NNNN NNNNNN NN N W- WN NNNNNNENNN -++.94NN NNNNN NNN"W94 .NNNNNNN N N NN.+ "N NNNCUCUCUCUCd U NN" I ( IAlNNCuCu('73) I('C7t'3('3C7('3('3('7('7('7('73('73('3('73('73('31('3'('3('3(13t"3('('CCUC('3('3C)I. + + ++4.InInInInInInIn4.tt CInSInIn,t ('3("('d.InINtr (nCVM C)('3 ('3m PC('3('3C)('('(v 4.4.4.4.4.4.4.4.4.4.4.4. 4.4.4.4. 4.4.4.4. 4.4.4.4 44.4.4. 44...4444.itIt4.etIhf~h ('3("t" NC) N NNNC" N NNNC7 N NNN N C(' CU CUUCNN ('N NC3 INN NNN MM N NN NNNrd- NrdrdrdrNNNNNNNNNNNNNNNNNNNN Nrd dNNNN"- ... . N (W).- - . , N MCU . - ('3C++ + ++U) ++n +n +n d+*+n +In +CV +t .+M +4('3 J +t"'+'3 +t'7+' +('+('3+('34.d +d +4n+4In+4n+4.n+at +CV) +++'3++('3 +( +('3N ++C +('3 +'7 +('3 +d +4t 4.4.d.4s4.+d +d +d +4. +('3 +(' C+N +N t'7+CU (')3+CUi (1)3+N ('3+N t"1+N +N +N ('+CI3++(V) CU+('3N C++++ + $PRINTCHARACTER0 LE0. 00001 0. 25000. 50002 0. 75001. 00003 1. 25001. 50004 1. 75002. 00005 2.25002. 50006 2. 75003. 00007 3. 25003. 50008 3. 75004. 00009 4. 25006TUranium Pseudo-Contour Map - Waycross QuadrangleVALUE0. 00000. 25000. 50000. 75001. 00001.25001. 50001.75002. 00002. 25002. 50002. 75003. 00003. 25003. 50003. 75004. 00004. 25004. 50004. 5000MISCALE IN EQUIVALENT PPMEXPLANATIONfIH3wbWAYCROSS.010A0'0'0'.0.0.0.0.0.0in4tqt.0U)1)UUnUU4.4.".v4.4.4.4.d'4.4.4.d'of4.'QV'4.4.4.4.it4.*44t4.4. 4.4.V4*. 44.4. 4.(6) mV4.((63l ( M 6M )62'3(6)1(6) (C7(62M6 c'('3(6I.V'4.I.4.4.4.44.4.4.4.4.4.4.4.4.4.4.4.4.4.4.4.4.4.4.R t44.V4 4it4.4.4.4.4.44.44. 4.4.4.4.1)et4.')4.4.1)4.4.1A4.'IA4.I)4.4.1)4.'.',)4. 4.4.4.4.4.4.et 4.4.44. 4.44. 44.44.4.*4.4.*4.4.1'Ot 'a d t ta'4 4 4. 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C7 CIA I00101C014.0000'0000'4'4'4'4'4'400000000000'4'4,'4,'4,'4'4''4'4-4'4'4'-'-'400000-','4W4-4'4NNNNCNCNCuNCNC94,'4000000000000000000OOOOOOONrdNNNN'4'40000000'---'4.I 4S44.-«- .'44.4-'.-4'4'-'4-4-4'-'4'-'4'4'4'4'4'4'4'4'400000NN N'4040000000000000000I -''4'4800000000000000'.4'4'4-4/ 0000000rdU)C')rd Iru 4'000400000000'-''4'4'400''4- ++ + ++"-+ 0 +Cu' +C') '4++0 N +q ++th +r, +4 +01 N +N N +4N +C' +Cu +C++'4u +W4 +'-'4 ' +' 4 '+r4 +++'4 +'4 +'4 +O +0 +0"' 0 +0i 0 +00+'' +r1 +r +In +0 0+'4 0+00+000++'4 +-O +S .- + ++1+.+C'C. +'4W+.+ -4 ++000i +'4 +1 '4 +' 4 +'4+ +'4 +0o+S+EXPLANATIONPRINTCHARACTER0VALUELE 0.0000'4000'4S 4'44-'4--. o0000tttf7 9.7500 10.500010.5000 11.25008 11.2500 12.000012.0000 12.75009 12. 7500 13. 5000GT 13. 5000Uranium/Potassium Pseudo-Contour Map - Waycross QuadrangleI0.00001 0.75001. 50002 2. 25003. 00003 3. 75004. 50004 5. 25006. 00005 6.75007. 50006 8. 25009. 0000i0.75001. 50002.25003. 00003. 75004. 50005. 25006. 00006. 75007. 50008. 25009. 00009. 7500iNN..iiiiiiiitIiH6wbWAYCROSS+4.4.4. ++++++4.++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++4.4..4.44.4..++.+++++++++4. +++++4.4+++++.+.+++.+++++++.+.+.++.+.+.+.+.+.+.+++++4.+.+.4.4.4.4.4.4.4.44 444U)U)4U) In U) IA)it' it4 4 UU i ) U )IA)U)et44' f U)44U)44U) U)4P 4 In U)4.4 e1'. 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I V4U)N 10 ) d ) T nn 'n IT NVnED N'O4 dC') U ) n ) )d nOD OD e r ) C) C') )nEDEDN et rd n)'O 'O n ) C') nN 10 C')C')4 NN'0UnUn)UnnU)t ') NN U) Vit N N U)U) 4n4'44I'0-0' ardOC'4U)444 4rdC') IU)(VC') VCd 1CS)4U)Itd'UUUU)UUU)0In0 U)0 N O 44.t U)o 4U)U)I4 EO D 0 U4t 41rN D%0 0 t").0 mU C') C) U) Cd0 0 '0 4Ut C'd d*N0 nOU)%0'0'0U NNC) 4N4 '4C U)4.Cdo V-'4W44000~4.4.+4 . v4 4r" n v **n4.. '0InN '0 in )4t4.4.UnN '%U)0U)0Ino d n in n,"00.0 I n I44 'CU U)U-0in , ,0nIn NU UU)o4.n n'OU)40.-0 U) iUU)U) U N 0U4In In 0O n o 0 '0 4vv n n 0Tet 0U) )4. e U)U)O'A U)c .oe ett' tt"*1 I retItnr) 4t a t iV') vaiU UC') 4)4t 44.4Un 4e4tIn Cfi t ') 44.V 44U) t44.t ) 4t4t4U)44 C') f44 It* n etU) n 4 . 4tIT 4.)4444r) ) 4 .4 f44 U) U) 4 tV49rd U qt4 4Cd d U)U)nU n4NCd'NNrdt')C')444.NU)t mCd,C)10 00'4'4'00009'4.Un 444I.EXPLANATIONC,)C)fia.4PRINTCHARACTER0U)InU)U)InInInI)UnChU.-U).4eU)C')Cd,.'4'44 C) C')C)C)) Cnt)C') C') C') C') C')C' ) C)C)C)C)C) C) C)C)C)Ce C ') C')1C) C )4d')C)' C')C'4t 4. C C)it V9) (llC)qt) In rd Cr)C) ')C etoCU'd C)C)ch4t 4 rdCd 4) r d) 4C') Cd'C') CNM N 00. 00001 0.05000. 10002 0. 15000.20003 0.25000. 30004 0. 35000. 40005 0. 45000. 50006 0. 55000. 60007 0. 65000.70008 0.75000.80009 0.8500VALUELE 0.00000. 05000. 10000. 15000.20000.25000. 30000. 35000. 40000. 45000. 50000. 55000. 60000. 65000. 70000.75000.80000.85000. 90004+ + ++ ++ ++ ++ ++4.+4.+++4.4.4.4.4.4.+4.4.+4.4.4.4.4.4. ++4.4+ +.4.4.4.4.4.4.4.4.4.4.++ +4+++4++4+.+..+4+++4 +..44.444+...4444+...444+.4+ + + + +Uranium/Thorium Pseudo-Contour Map - Waycross Quadrangle44444++++++.+.+.+.++++.+.+.+.+.++++++.++i1 _. ... ..]aiii{11f17:++++iiiiIII'H7wbWAYCROSS+++++ ++++ +++ tt t t t t t t tt+ tt t tt+ tt t t t t t t++t++ tt+ tt+++ t t ++ t + i+t t tt t t+ t t t tt tC) P) 4444....4444It) 4t44.. .44C)C) 44.4'C C)C) C) 44'4' 44MM Cn w )i))C)t"C) 444 U eU '4.C)Cr)C) 44'4 ) 4 .4 C A)C)C C) M 444.4 ( N C)C C) V 4.4.'rt)t Mv4. C) drCC) MM~U) C) rCuIr u C ( u dC)C)C1r). ) NCu Cu~u duNu CC44'4 r) Cu udu u Vuu r C4 d4' Cu u Cu N u4000 u4. C) tCu) Cuu CuuPuu)C) CuM ff N NCuu uuV)C 4 u C'C) rdu~~~uu~~4Cet4) MC N 0 N uC) 4444 M)) N)-Cu "- 004 4.4. C)C) .Cu -004t t )C) N + Cu-0 04.4. CC)C) u- 004.. ))C 0004. 4. )C)CN) Cu W-4.4.4 C)C) C 0 Cu)4t 4.4.4. NN Cu -4. C))t uNNNNNO4. C))C) u Cu.'0 oC) C)C) CuOOC)C)C)C) Cu - OO4.V.4.4.atIC)C)lt'7CCV) cnC)C)C')CCCryC7(3('34.'3B!InInInIn1)U)U)InInU)U)eh4.q,4tqrRtt?4.4.4tetqrC)C7('31(')e 'goU'0U)U)U)U)U)I)It)N 1N)U'0'0'0D,a''00'4.4.d'4.4.i a' "Ua d'4.4. d4.odU) 4C) Cufi r r rC1C) CufimC) firdmC1 Crd rdfm NN rMMM N NNdrC) C) rdufi rd CuC) C) C) rdird rdfrC))C)C) Cur ru ufi-i C ) C 'rdC rd ud 9 -IC)C))CCVINfi Cu -dC)CCC)).ui -C)C) fifE -$" W4 V4==C) uNuif -- MCufiMMu=ufififE**~~Cnnnn 4..40n nn' 0n*0''0!}n dIn VO0' 0CInm 0,CuN ('3V)N N CNN ('C)NN ('3) *V))C t"MmmN0m4.U)4.to4.to*.4IU) nN.NNNNIo i'0"0 o'00O0 OO1O00CC)00101010101010101Cuin.4 ..4 ..4 - -- '.-.M- - 4-4 f------ W --4---r4-4 400000'-4.-+.-'-W4Cu4..4---. 4-. 4---. 4v.4 v4.- 4.4--. 4.- 4r4rd'.rdCud iCuNC,3O000000000000100,0'.400 itCCOW NU)0 N0'hlN'04.N'04.0-010D'0U)'0InInInq, q et4t t 4 , -hmIn .4.4.4. 4.4.U)Uin 0NOO] 0'4nn 4 4. NN 0.o -00%00) N 0''0''0'' 0 NCO0%N '00 N 0'NN 'O-0 N N ID"N '0 . hN CON4 '0' Nm C'0 0'0 N'04 NNNNNNNNNNNNNNNN NNNNNNrNN N NN NNNNN NNNmNN N t N' ttmN 'mt N))( mVmtt)C0tmmtt tt )VNCuur NNuNNNNNNN rduNud C) uf CuNuC Ni Cu ('0 C')CNNN rdrdd NN NN V 0v0000 V P) PNu C Cu uu1uV NC )NNNNNNNNNN C)C(.4- '44 .4-4NNNNNNNNN.44 .4 4 . 4.4. '.4, .4 N N N N N Nu~u~..+4-+. 4.44W94V.44... NrdrdrdNNN000 0 * "+- i. 0 -« NNtN NNNNNN N00 0 0 000000 '4 4,4, '.44.4 C Ci -C4uuu~~0000000000000000 .4..4 NNNN NNCNNNN000000000000000000...edCVu urCudu uNNNNNNN00000000000000p000 W4 V-4 NN NN NNNNNNN000000000000000000000-- C.4. N NN uNNNNNNNuO00000000000000 00000000.+-"CuNNNuNNNNNNNNN000000 00000000000000 "4.4 NNNN NNNNNNNNNNNN0000000000000000000000 - uNNNN NNNNNNNNNNNNNN00000000000000000000000 -t CuuNuuNuuNuuNuuNuNNuNNuNNuNNu0000000000000000000000 "-4 CNuNNuuNuuNuuNNNNNu NNN~uu~0000000000000000000000 - 4NNN000000000 +-- + 000000000 '- «i+u0000000- Cu Nu00000000 - C00000Q 0 4'3 CuNi000000 --. CuNu0000 -1 4n Cu N 0000 - - Cu000 -+NC'0 ' '0 4 0 . - 00 0 900 .4NCu4t .U0N N'0 Cu- 00 -. q0 4 .U)' r N0N CD3('3 00 4.4-- C~o. NW 0 (Pk(. 'o 0 ('3 - Cu Nu -- CuNNuNuuNuNNuNuuNu.4-CuN 'ON 000.0"4.Cu-- CuCV u l -- 4 CuNuNNuNuNuu~uru uuduNud.4 4 N O D 0"O (%') NCu -. 4 NNNNNuNNNCC) -0N 0)0.0" oN Cu N NuNN CNuu")C)C)C'3 0)Cu n"ON 0(0 0" 0 '04. Cu uN CNu N C )C)C) (3CCu n) N 00303 0" 03 q4. rCuNCu dCudurd 'C)('3 4r4t (')Cl'.w Er 0C')3rdurd CVC)C)(' 4. 4t C')C7(C3C7 dInNON'0It140 et it T Itn int Itt I it a ' tC) C% 0'n0m l, n mNU)~C CD).. )'O0.0 .4. %4.4.n 1)10NU)4.4.4 1)1N$ 4.44..4ON ON ON o Or'0U)U)'0 NCOO'4DOIn In)In'0 0'it! In InIn IninU) "O n'0 '0'0 '0 '0 '0N N'0'00' 0'NU)ON0'0ONCOCOa,O 00000 NNNNN 'OmW'0 U)01)U)W fn)in I'0InCOnN'0-'4 0000000000000000000U)'0Noo4.4.4.14.4 1)4.4.U,N40n ND% 4%'0 N.o ''0''00'-0O00-'0 '0 0- 0 0O . "0"0%01010CIOInU)U)if!InInIt)$4.C)C)IA IItC)M)('3vr, NCI N NNNN NNN NNrdNNNCuC) CIC)C)C)CC)C)CCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuNCurdNNNNCuCuCurdrdCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuCuIt)t. C)'0 4. ))N'0 4.'0 4.4.4.1)e4.4..4.4N.'0'0'0nS'0U)U)U)1)A iU)U!1)IA 4.U) 4.U)n44. dC)C,)C)C)t'C)C)MCC)iC)iC)ionn 4Dn 4 n'0ONam'0U) NU)'0'1)U)''04.n4.*4..UC)CtC)C)t"1 C) )tC))C IC)NCNCNCC?C7t'3C]C)C) Ct" "ninInininInMInInf + + + + +iiiiiiii00+n++SC))+('3++NN +N" +NN+NN+NN+NN+NN+NN .NN +N +N +N +N +N +NC +N +NC +N +CN+N +N +C +C) +mC+C, +C) )+et ') +et ++40 +44+I+-0 '0 +0 ++0 +'0'O+0 +S++0 +0 +'0 +0 +U)'+U) +4.4' +4. +0+C, ++"3 +('3(t') +('3C)m +C) C)C) ++4.4+ +Residual Magnetic Pseudo-Contour Map - Waycross QuadrangleEXPLANATIONPRINTCHARACTERC) CCCCV))ry) C ))CVm(m'0 CC C3C)C)m 0Ce C) C? C)r mUe4. 4.4'04C)C C)4 1)1 1))nn etCO C) C)4.U) 1)1)nn 1)))n C) C i nnnnnIan C t') C)C) n n n1 )n0'CO0 C) C) 4. 1)1)n1n)n1n)tN 4. C) C ) 4. 1)1))n11 10,010'0 1) 4 C) *)C) 4. 1 n)n ) ' 0 0CON CC C)4 1))) ''0 4. C)C)W)C ))4.V nn 0 '04. v C) C)Ca) C7 4.4.4.4. 1)1) "0C 4.4.4.4. 11) 0nn '0'Itrr7 '(V )th et4t V nn 10 4aM c r$ ' t t $ V nn 14 Cu C1) 4. )0031)1)os ' c') t* nn nU) C) CP)C) 444. 11)))1110 C) )C1) )I4t.4.4. 41)1))10 4rc) ca) C ) '4o4. 1)1)Vit tn htV1)1 Ogt itt *eNU)4. )1)) ) 4.4.t trfit10n MC)C)CC)CC 4'0t C)C )C "C 4.e.4et4.4.4.4n 4. C)C*)CC)C 4.4 4.4.4N 4. C )C)) 4.4 4.4.4.4.4'01) itC tCr).4.4 4.4.'01).vCC)CC)CC) .4. 4.4nUU)onnn1)It4.4.44.404.St4.'q.II.VALUE4 (()C('3C)C) C) C)C)C'3)C)rmC)C)C)C) C) C) )C) 'C) )CVr) Cl) )P)(C) C))U)'0U)NSuU)U)U4.q4.4.4Tt?'Rtgr4.4.4.4.'4.4.td'4.4'qrd'4.4.ItRrd'iti.4t4t4tIt4.4.It4.4tq'LE-1100.0000-1100.0000-1050.00001-1050.0000-1000.0000-1000. 0000 -950. 00002 -950. 0000 -900. 0000-900. 0000 -850. 00003 -850. 0000 -800. 0000-800. 0000 -750. 00004 -750. 0000 -700. 0000-700. 0000 -650. 00005 -650. 0000 -600. 0000-600. 0000 -550.00006 -550. 0000 -500. 0000-500. 0000 -450. 00007 -450. 0000 -400. 0000-400. 0000 -350. 00008 -350. 0000 -300. 0000-300. 0000 -250. 00009 -250. 0000 -200. 0000GT -200. 0000- - r-.SCALE IN GAMMASH8wbBRUNSWICK+-+4.'+ 1+.'4.'++I++++.++4.+++++++.++4.4.4.++++++++4.++++H9400C)CD"08094CDrdDrdCdCdrdI InC'14V-4---944rd14,a4N0OD46NID94 .W4 N N W4.,- rd rdCdrd -.+ rdrdrd -V4944rd rd "". " +N N9444 Cd Cd .4.4. N N4 ...4 4 N N 9..".,4« N (V .4 '4.4 .4rd rd rd 4 4 4NNN N r ' wN N C) { 4 -- .Cd~~d d 9944 41Cd' NIC')-44 .4C..C.,()N .49..4() Md W4q4q4N)14. C7 ca C') M 9N 94944.1 NN -Cd4'NNN N) CrC)C)d 9494~Cdd ( d InCN N)C ) CU"'IN C') I.... Cd C)Cd IW+d ") N o t.U'4.-N4.U)C,nU)4C')Cd-rW (..44.n nnN4.nd4'44949NNNrd944,9f 4Sd'C')S.nIn.4C)U)rdt'CdNtNWNCrNd rN4.fU)1.0.--4rrd9999'0t")4.4.I.1.."U)0 ASU)InNi UInn 4.iNNO 4.NO 4.4 04.0 0 IUs) .IA d'.4U) 4.U)4.4.IA d' CIe! C') (')U)')4.*4.n0 1 4e4.104..0 U)14U) U) 4 fU0-0 NO D D 4.4. O0 ODNtt4D '01 CD ( 4. 4.Cd nn ONN DOIOD 4.4rd U) Nt4.4.rd n 44Cd )4 OONCd -40N( O' 'D1 0 4.1( Cn N N iN 4.n '0 WN CV) aan.0* aa4t*CN1C'NN'nn as ait ai aaU) C U) V C(.on lO U) 4.C1)CN4.40 C1N4.4..4. 4.43 C'Ca0 e l) CdNd('7 4.0 It)It) C') 4 .4.Un U)4t4 C') I 4Ui UU) r N M C't 't t m -0in m rd N PV"It . "Un NU)' nC) l.l. NU) CN C)ln 44On in or * *U)it~ C') 4et .U non 0a' In ed)lU ) d V ' V' 4..'0 0fU) CIA NC')e 4.4.4.10IA U) tCdto V) .. 4Ute I ) C C) 4 .. t1. C C CdC) 44..C) N ' 0C"'Cy C'! ) M V' 44.C C C') C ) 4.U) N 44.C)C)C 4,OUot 9t 2eC1at eNm ..nC') c') 44(2C) (N) CNC')Cd94U!II)A deNe C"0 -.0 In qt( ')4.flU)t094Cd949494rd rd dCd(')00 94-IF f f t f f f t f f f f f f f f t f f f t t t f t t t f f t t f f f f+ t t f f t f f f t t f94-494.04.0-0 -C0'0 10 'CND N U)+4.4.+4.4.++4.++4.+4.4.+4.4.4.4.4.4.4.4.+4.4.+4.4.++4.++4.4.4.4.+4.+4.4.++4.4.+4.4.+4.4.++4.+4.4.+4.++4.4.4.4.4.+4.4.+4.4.4.4.4.4.4.4.+4.4.4.4.4.4.LE 0. 00004.C,Cd949494QT 0. 4500Potassium Pseudo-Contour Map - Brunswick QuadrangleEXPLANATIONPRINTCHARACTER0e.0r3NOCd N()4. 4MU(I34.1VALUE.0N94C9494940.02500.05000.07500. 10000. 12500. 15000.17500. 20000.22500.25000.27500. 30000. 32500. 35000. 37500. 40000. 42500. 4500CdrdCdCd94949494.4.4.494949494I0. 00001 0. 02500. 05002 0. 07500. 10003 0. 12500. 15004 0.17500. 20005 0. 22500. 25006 0.27500. 30007 0. 32500. 35008 0. 37500. 40009 0. 42504.IIIi9iiSCALE IN EQUIVALENT PERCENTH9wbBRUNSWICK('3"('7 N(.3 PM.(3'C'1(C1('3Q '34. 1N U N wM W4NM MM) .4('3(3('3 949Mj~4'.44.4. M3nru '-4.4. qt ('3'3('4 it d'3M ) ( rd rd'it C')qt t rdNd r4. 4U ( t'3 ( N Cry't')N ('34.. e Vo.n ('3 m(+-'' 0 0 '4. 4.') t C) )Nv40 9'34.4.tel .V V' V) ('37 ('3 N .40 ('34.4.('3 *4.4.Cy(N - -4 ('4. 4('3 t") to.V" V4. ('3 ('N N (3). 4.(' 4. ('3 i 4. ('3o i(' C)N In I . .4(NN ('3 i4. C '3M U) ' 4 . N N (3C) iit(' C')3V" tinqVN C)'N (')N N (') In '. 4U ('3toC94. ('34. 4.in NN('e N N t rd 1r N CO V C i iNc cu m r, V a et Ia n (' N '3 .) 4In (' n n ('3In N N'3' N ('3 4.4. 4)In (' nIn ('3('3NN ('3 t") 4Cin (') iC) N a IdNCC) r m Bch U)U I('3 Nft? ( 4 ).Cn ('3V 4. IinN t N ( ' 3 4 . 3N 4 .4 . 4 .N N CN'3('3 4 4.4. in4. INN C')('M N 4.4.4. NNnn 4.4.44 N N N) (rd NN 4 I n 44.'NeN N(' ('(1 4.44. in4( ' IN NC ('3 'N3N 4. In 4.N ('3 I N N(' ('3 4. iniN('(3 ' ('3 (' ('(3 4..4N ()3 C N(N( ('3N (' 4.) 4. 4..4.C ) ) N ('3 N N 44t") n.)C) N('3 ) 3N '3N N(V('3) 40.') I 9NNm rd3'3(3N N '3 ('3 ('INit N.N(' NNN .4V'N1 ('3 4. NN -- tN3 N 4.( C) nNC(' 4(W) C) C)NNNrN ('3 iU) .P) NC? C) C) C) C) NN 1 ('3 in 1 ('3 N )( C) C C)C N N -0'-0'34.1in N NV('3 C) C )( ) N (Vm N) ('3 1 4.(viV4.4. (t"1'3(13 N .. ( N N'3CI ?4C.4. C)(N) C)3 N (") i 9)3V4P4. N4.U4CD).4 N ('3 NN 9494 n N44. 44447 ('3 N 9 I n '.4 3( 'NN "44 .- 4 ( ' 3 i n W4.4. it3(3N3 N C) It InI i t ) N('3Ni(+'3 V ('(33'N 00 iVtvn . '3N ('" ""C7 )(' (' ('3C) 0(13i4. i'0 N (v NC)('3rd mNn9-4.,9W.49«.,4.1.-4.-1W4419. 9.4'94'4494rdrd94949.4rd94M'N4. NNN(d '3d.IC'('4. 49494 ((n C (' ( '3949949 ( 4C'3 C7 '73 - - -4t'7C3 . ('3 N. 4 N4. ('3 N N-- CIn 4t (3NNNNNIn VV dN N NnV'CC') NNNC3C3N9in ( dr dM~dIfn N NIn a CV) NrN rd4V'..4 94It.a4 9 w d . 4 941 V944 94Ii4 ('t 949W494944.4.4. (V3N.-4w-~~rd C'3 W43N 9.4'-r949rd. .N .. 4 (r+.C.4 . 9+49.44N .4 .44 ('3( CV ('3N 9 .,4-('dN ('3 '94d4 4 .('NrN W4 94d94 NN4 44Ce9N 4 rdC'3N rd '+49W4 9- 4 NW4 W4 N9.4N 9.4N++++++.++++++.+++++++++++4.+++++4.+++4.4.+.+4.PRINTCHARACTER00. 00001 0. 25000.50002 0.75001. 00003 1.25001. 50004 1. 75002. 00005 2.25002. 50006 2. 75003. 00007 3. 25003. 50008 3. 75004. 00009 4. 2500VALUELE 0. 00000.25000. 50000. 75001.00001. 25001. 50001.75002. 00002. 25002. 50002. 75003. 00003. 25003. 50003. 75004. 00004. 25004. 5000GT 4. 5000Uranium Pseudo-Contour Map - Brunswick QuadrangleI,W+ NW4W4NN)EXPLANATIONSCALE IN EQUIVALENT PPMH10 wbBRUNSWICK+++++ ++++ +++++ ++++ ++++++++ ++++ +++ +++ +++++++++++++Cut7n'+++++++++.+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++U) $. 10 coon '4'$'-4Cu nU) M)t(4, 4n) .01')C'C) Cu" i "m V U)U)If4.)(3 4t '. N Cn) W M('3(V3'3 N4 OnoUU)U (')(')44. «.. RU)4-nU4 0o4 4.. )I 'u n n i N n ". n it C , ' n n it qtN "t nn enit in n itC) It r C)et'q t N NN i "q at in C) N N "4$0 n i CuNU)et U) U)Uq 1r )n10 4trd C) n 0 %0) q44 1)CUCUMCrit 4 itU) 4t'3CuCI -)0 4 .% ( ')CU Cu"4"44. 44('0 min et0netcm U('3U)0 '0 4 t') ('3 r('3CUnet 4 C) net Un CC' 'Q 0 409 0 ('3 ('') C N q C44 3' ) 1)4net )4. uh 01net)4 (' ( i3 N CC~CI (' ('34 1)4 lCU4. th '04 (')(it ('3) (NNu~( i((') ) N1n 4. e4rd N. 001et.t') M'(W)1') Cu 1))4.4tCUN n 0n)4C) C)( 'N(CuCU ) to N ) 0 U ) t' '00-n (N(N+CC')qt nCu '3 et et' n 0neN NNog (V)CCICV ('3 4.4.1) it') n )001)nnqU NU 94 NN q' 't q ) t4t q 4 n. (,4 CC ('34'4.44 441)n 4.0Cit "'C) C' ) 4$ 4 .4. 4 0 1 4 "y","4C Cu NN4 I 4.4 1t) 00 4 "4 o "+('3(1 ( C '4q 4.tn)4(4.iUn '0 4. 44. "4 " 4. "4C') C') e 4(c) n) n) n in et"4Cu (W)3O444t1C3 CI n n n n CUCNNUNUCu C)'3 t it.4.4it Cu ('31') 4.44t 1n n n '010 4(W)Cu ('3) 4t 4.4C'3Cu (VCf) 4.4t qt nn '0 4. Cu NCl) '31')) 4 .Cu (1 .3) 1 '0 tNetS4.4. ')C CU ( '3 4(m n CU., )Cu u (,,'34 N CIi 4(1 .e 1 a 0Nu 4.1)1)t') NCu C le('34.1)4t "0.0) Cu CuN 4t .* (3m Cu N n f (C NCuCuNuC') n ('(() N u ('31' ('3e rnCCu Nu(') r) rd rd N C) it n('3 Cu 4 CuN Cu*CIu I n1)4.l "*NN ()3 '%0'01n)4 C)NN C)4 CuU)'Curu rd NNN '0 4(Vu(3Cu Cu1') 9)) 4.('3Cu Cu Nt~U (1) n'0 (1C)udC V C(1) CuCU Cu ( 4C 3('341)1)4.('3Cu Cu u~u 4.1"0 .0 1') Cufl CuWduNu e4Unn*).(13Cu uCu ' U) (nCuC-U uNNet n q 4(3Cu NCu Cu.0 1nCu Cu uV Cun itg N * n%0 10,-%0n I -NMEN4. in it *4) Cu 10 0 0 1)4 .0 (r7 C (N CNnn it qt. 'Cu 4. 0'N14 n CI u ('3Cun n 44 gen 4. 01))er 4. cUC) C)+ + +U) ++ ++ +'3CI +++0'0 +++ +++++'3 C)Cu C )it it 4 ) VCu 0D1) '0'0 1C) 41) 1)1') Cu C I4t ) 4 ..13Cu U) at h %0'3' Cui ('31')netU V44() NCI (IeU) 34( NC uu (144.C' ('3 NCUC) '0 h 0))('3 U) FNCN9t4 r)t*1r 1('3 rdwt N '0 NNN -4--4W4Cun1C)C 41')u('N0.?qE N CN u (V '3W+ C('3(134.N1''0 .01k'0 n NC I~~ ""C) ('3et %0)"0 C) N C CU r+ "N('34 n 4n Cu 0 0 't U) ( td (13) N "4+('3 ('3 4 '0nn0 n (')CU 'Cu 4 "Cu+ +1)+1)+ ('3++ ++0++0++ ++ ++ ++ ++ ++ ++ ++C++ ++ ++ ++NNCCudrd"4W4"4..4"4N4(V)('3('3Thorium Pseudo-Contour Map - Brunswick Quadrangle("'4.4 4.4 In1)4.C( N'3 ('3Cu I(1)'9It1NI.4 CuN 10 qt f Rr l'4.11r 1W0 4.4a'.d'3it "'"4NCud) 0 44?4I.CN()3(Cu"I~"0 ('3) Cu4.1)In 'Cu CuN U)n Cu++++('3++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++4.VALUE0.0000PRINTCHARACTERS0 LE0. 00001 0.62501.25002 1.87502. 50003 3. 12503. 75004 4.37505.00005 5.62506. 25006 6. 87507. 50007 8.12508.-75008 9.3750 10.000010.0000 10.62509 10.6250 11.25006T 11.2500SCALE IN EQUIVALENT PPMEXPLANATION0.62501. 25001.87502. 50003. 12503. 75004.37505. 00005. 62506. 25006. 87507. 50008. 12508. 75009. 3750rdaH11wbBRUNSWICK0000V40 r+0'-Os -00'4CuS)NCN090-90'-000000000000000 r+4000 0 0 -W4 C9449 C.,4.4+rNNNt"- NN 'On.0 .O94 ('3W'.4-94e U)t% N0UO '0 '0U) '0 '9494 0 00W''0 I'n10 10 N0 C0aflU)'1r)Cu ("C No)v)4. CUCUN00000C') ) U) ' CuC)n n e zn N c1 n it rd rd IV' (V) it(V)4.NCu C(')C) a 4. U) 4C') Cu C)(FC') ) in r%'04.V' dCuin ItC') U) ".'04. uC')n.a004.i " NC) 44.4 '0 C CVC')-0-0 we .41n 0 CuCuu()h" ni U)Wi CV)Cru Cu'04 e t i C'm (n)C CunU). C)C 4.4.C)) Cu u u4.N n (w) rd c m N dh ) C,) tCu)4C) Cu4n"t. t") "-+ C) (') C') tCu1O .O M C') (C' ) CuCi0 U0C') 94- Cu C)4.'()Cun .0 n C)C CN u Cn n ~ N eV4.. 4. Curuu C')4.4. ') nU)'rdur t) C) (W)4. (3(V) m n)NIV tvu N mwe t3 C'n CI rCurP) ('3.4 CuCC') Cuo C') Cu ')CuCuV') r Cu!")Nu CCuNN~CuCu CuCu Cu CuruCu Cu uNCu94.,9494.4C')t"?N94CuC')9494Ne toCuNuN-49494+ 4C') u CNN M NO4nC' 4(f Cu.a 4.4.a Cuc u '-i(ur dRt t drd M d dYNre ")C)U) 4.C ')dr d d IdC C)CuriC rdu C4.cor C') C'C'C')u Nuu4. C' (I r ru Cu CuCuNr'V) C') m u rd Cud CuC)'M(V) Cu C urd u ur uuCr+ '.0 ) C')CI Cu Cdu (VCu u,0 n et Cu C C') aaCu Cu CNU Cu M C') .CC C u Cun tit C') 1) v C rd rdCu')C' )C)C' Cu Cu -'0 ( CMP'C'C ) ( Cu CU) 4. ' C)(C') ( Cu Cu 9dU)t )n)n ') C) C 7N rdC' Cuit n)nCU rd C') Cu4 U nn t' C C'C ' Cu Cu4. W)U C rd rdCr') 4 Cut4. n WW4CCuu.u u -C4. n et). Cu4 gU ) e t 4. -4 94U) U) 4 9 4 9944.4.4.4.4.+flICu +.4..4.++++4..4.+4.+.4.++++.4..9.+4.4.4.4.4.4.+4.4.4.4.4.4.+4.4.4.4.4.4.4.4.4.4.4.+4.4.+4.4.+4.4.4.4.4.4.4.4.+4.4.+4.4.4.4.4.4.4.4.+4.4.+4.4.++4.4.4.4.+4.4.4.4.0 LE0. 00001 2. 50005. 0000VALUE0.00002. 50005. 00007. 50002 7.5000 10.000010.0000 12.50003 12.5000 15.000015.0000 17.50004 17.5000 20.000020.0000 22.50005 22. 500025. 00006 27. 500025. 000027. 500030. 000030. 00007 32. 500035. 00008 37. 500035. 000037. 500040. 000040. 0000 42. 50009 42. 5000 45. 0000GT 45. 0000Thorium/Potassium Pseudo-Contour Map - Brunswick QuadrangleEXPLANATIONPRINTCHARACTER04 PCf')4U)4 0 (0 0(1)Cu 00 U)C)Cu 400 '0 '0'-00 410 '01C') '04t ) Cu NW '0'04(V -e -4 t')"0 '04. N -C 0404. 4. Cu N N W)4. 4. C)C Cu UC) .4.e C) - Cu U)C)C'3) d 4. ') '- 4 4s .CI toCuuu . CCr U)" " " * C) * U)94-'C-C' 4.-949 C' 4. U)nNNN)InC7f I1.49494N94.4C9)t4.4.4.C'CuCuCu' "fNCCuC').o'04Nth- C')WM'u-4W4.- 4,4000 00000000000000000044W.4.940940V-4.9.9.-.4un-N0 94094-O r+C «+9.4.-4-494900000000094Cuc)4.in0000000C')'094-0 drd rin me443"'a'0'0n0O0W40O0000nU'0U)(V)Cu9400001CuC)C)+ NC')t it" N)94CI4949-4-W4W49W4(V)C')0CuCuNCuCNCuCuCu94Cu4C')1r).400.4CuP)4.4.InN9-408094CUC"4949494194'-I0Cut"C')U)'0N".H12 wbBRUNSWICK94.-4900000000000000.uNCu00.00000.- I0 0 4-4 00000000000000000000000.0'-14dNNO0M1Cururd r-I00..g0W49400094CuW4 (1).-0 N94n9-449494., 94- -4NuW-Nu .rd rcC7U)( CU)4.4.4.U)4.Cu-4[UM rC)1 04.'S0"D10U)94Cu94Cun (3400009F494949494000000.4 rd (13)Cu0 94o094r1-,-4-499-9W494-- 09 400t"1 C 0904t P) v4 04. 44t(13 (13 Ird 9S N0 NC uCu 4rdo I0t")(13(13ururdrdrdrdrd'-.-4-.- .-ruurC)00094W4C)In0N949-49 4'-.-00.,00rd-0'094CuCu4U)101094Nuru Cut' eIA OIA qt trdir Ot itrd rdel () I- V. rd rd (w- rd rdr d "Cu N NW4.940000O.o4N IC1Cu(13(1)094Cu(134.4.000'40W4 00Nu094(13N1'3rdU)r14.Cu9494'U)eIA i( U)( 1CuNerd V)..,00-400.000000000000-4999illrdCuwuC)CuCuU)94o U(13UnU)(13Non4040U) 1U) 1U) 1U) 1litU),U) 0N ,o)10ION101010101010101101010101000000000.,rd[*Iet4..,Cu(V)4(13C)(I)rd ICu4.CInI40ICU00-0--0.0-0.0 .101'01'00-0lOICaN-010U)InIninIn.0NNN99400000094U)U)4.4.(13(134.'0NCIODN-0 -.00INU)INUU)1010(t1CI9400000rud iInS13CO)(1()(V)"uNue4n'0(1.'0'0InIn1U)U)U,1IS4D in.0n10U-)0d U)U)U)00 tS )ItU)IninU)I)In 0IOU)Q'4.44.4.4.'4.4.U)44.'4U)Urd)4.4. (14.4(13 (13() 13(1)(13(13(1(3(314.t"1u94tCI07 (1mru rdW4 (13.(100.000000+4.4(14.o(13")(" )3 (V - 00(Q (9) '. 0. (3 - 0-0 U! it (v) N '-"0 U)U) () ("1N . 4.In I n ( )uIn In n rd d t4n0 r - W4et 0 .0 .4 '.4n.U)10 4 -it 0 10 0 o uf0.,C~'t U)1010 td 0 (tt40 0 N0 p4'-InInU) 40 0 U)(1'.0 .491 n 0 1U)(13"-O "0140 -0 (13-.0 10 M(V)"0F n N- -"-0 (') N -40In (")N ,.04 U) U a(1 m 09( t t 4(1) - 0. 4 E(") " ' $(") e 0 - 'et(")3 r C(134.(13 94 0+ NIt C) 0 0".+(")f+ 00(l)0 C) - 0 CNuNuCuOOOOO94O4. a C Ird( (34. (13C7 rduCu94-4-494.4CuCu4t rd - Cu.-{CdrdNu U)In000094CuCuU)N rd-40090000000000000000000000rs-Cu 94rd "-'-4 - 94"1.40Q.,010M ((13Co NM4- (1M C4 rd~C1W4NMrMNM"""W494 r.. 4'-'19494949494.4.,499494-W4W4-4rd(1CurdCuW4'44NICuNIrurddC,r,Cu0Cu9400N9494Nu (13 M 9(13 ,94949 q944-0o 00 '(uNrurdH94949494Inv v'-'0r1 0- o949494.- 4OO4(1300094et94194q0."1.,Cu940i+++94++.f +++++++9+++++++++++++++++++++9+++9+++9++++++9+++++++++++++++++++++9++.++++++9+++++++++++0VALUELE0. 00001 0. 75001. 50002 2. 25003. 00003 3. 75004. 50004 5. 25006. 00005 6. 75007.50006 8. 25009. 00000. 00000. 75001. 50002. 25003. 00003. 75004. 50005. 25006. 00006. 75007. 50008. 25009. 00009. 75007 9. 7500 10. 500010.5000 11.25008 11.2500 12.000012. 0000 12. 75009 12. 7500 13. 5000GT 13. 5000Uranium/Potassium Pseudo-Contour Map - Brunswick Quadrangle4.4.(13(1Cu0000O0000OO00n94U)CuCuCu94EXPLANATIONPRINTCHARACTERIIIifIiiiH13wbBRUNSWICK++.44.4.++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++'++++++++0W4CufifiW4 c) r,rd W4 W4C) -Cfinn -nfl Cu rfinn -C' '! Cur CCuIu Cu) Cue.4C7C7 C NC)C1N NiN,.,,.,d rdC in4.4 . 4 . 4 . nJ- So e Mo 0oC3 C7 CC)if( ) fiWt .. rd 0 C') C 7C)C'3 0 .,C'3 (''!t'4 ) -400 C') (')t'3 N '-. 0() N t 4 e h e dC') C 7 C N e00V'N V)C - - NC' ) W(C)W4 "V' o t 0 t * C7 N ) '') c70 C)4.4.t t4V4.t7.C)4.4it4qt (W) MC') C') f N U -,V'4 I')C') it4t 4 4. ( fe t') M N C C CV'4.4.I t C9)4. 4.4. 4t .t4e nfl C) Cu CuN Iqt U) (') C')4.s 4.q 4.4.' 4VI C)C' fCd rdC 7O n e it t V'c7 tN...,U)0 Vf 4 e. 4. 4t4C ') (9)C - (sti9 e NNen e et ' V UCN--,4t~n U) NNCUqt C)4. 4.t U) 4V' Cu- Cat'4t U))C U d t44.f ')d'. d'. d) 4. It4itCu'4 (,9c7 '"C') N 4. (( 44. 4. 4.4. CV'-, 94 N.-'N 0).V' V' Rfi4 4tN.-,.,a 4t N V' C3 V*qt 'V' qt 4 "N V 4. C 0*4.4.4.*4..4 4. ''-4-0 0 NN V' C) N)et *et V'V' t ii.. -'in CN 4. C) C) ) et4.4.4.4.4 . 4.4.V' V' CU N U V4. fi) .44. .4. (9)'4"-V' C7 4 e C) ) 4. 4. . -'C '4'4.C' Cu . )) C) C) (' NC7 '(')(' V" C')N C) rd V- N4. n n '. n onnn Cu Cu4(') nnC (r) . fi Cu '3 fi CN-,0 Cu(iC' ') 4't4C) N n ('3 Cu'40 CuC7Cnt) ItN C' C)C') rdi C nnn Cu 0 CuC3 t7 V'4. C )C) C)(")i d rdcm cm 0 Cu'C0 4.tCu 7 fi Culn ) NNNN - 0 0 N('3x 4. 00 nfl' 7C 7 VCuCuur 'r 0 Cu4.4. 4 it iflf fi fin Cu)u u)uN -,- 0 C4.4. CuN 4. nfn fi nn CuNu oNCUC-, 0C4.4.0r fiNCU)CC') Cu ifii C ) iifi Cu '4 .- 4 0"-4.4 it Cu N uNuN N Cufiift ii7f Cu '3r t V -, -+ 0d4 fi) CU NC Cu d fifififi fiC)C)N - 4 -,qtqt (VN N - N ne")") oCN -+V' C)Ni -uuu4 Cu fifrfiC ChfIf)i , - -qt C3 NVN - N C7M ) 7 C C -qt ir N-y-, ') o n m N+ -,(')(17thCu-N ifinfi fi 7 t'7 Cu'4 '4Cu NM C3if '4Cu fififi n nn Cvn f)Cu .. Cu ufififi C7 ' r r 9) CC iffi3f N C Cu'4-, NC)iC7 etfit('U')4. Cu'3fifiififiVf C rd fC u Cu(3C7 ' i C7C'3l 4.4 f(fiiffi NC C -'-rd (Va 2 n 0('3) 4.4. CInC) I C N)' C u CuNC7 44. C) C)(r fi0i Cu u N-, --CuC) N4.C fifi7ifi Cut--- - -,-t'7 it N 0 00r ) N -, - -,0, - - '-fi CN)CN9C C'fif)f ) - '4 00CuiC3 M N-, N 00C3 ) i-Cu 0 0 0 -Cu r ) (3 - 37) (V) iiffii-+CuN '400 -N Cf N faCC 7i fn -Cu N-00-'N4Ci (lNi c7 )f (9) '-4 '000 - fcN C9)fl 7( c7 fi fin uN+ + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + +N)CuCu'4''41., 1'4- I'4..4'4'40000-4NSC)C)- If+ N00-00'400-0040.4.4 .' 4 '4NNNNrdCuCu'4'4NNNC) Cu W4--.O- ( -4W4CNr1'4W4V4'40EXPLANATIONPRINTCHARACTER0 LE0. 00001 0. 05000. 10002 0. 15000. 20003 0. 25000. 30004 0. 35000. 40005 0. 45000. 50006 0. 55000. 60007 0. 65000. 70008 0. 75000. 80009 0.8500VALUE0.00000.05000. 10000. 15000. 20000.25000. 30000. 35000. 40000. 45000. 50000. 55000. 60000. 65000. 70000. 75000. 80000. 85000. 9000GT 0. 9000Uranium/Thorium Pseudo-Contour Map - Brunswick QuadrangleN PC)'Id'4.Rt4.a'fifiH14wbBRUNSWICK+4"++++++++++++4.++++++++++4.4.++4.++4.++4.+4.4.+4.4.+4.4.+4.4.+4.4.+4.4.+4.++4.4.+4.4.4.4.4.+4.4.++4.4.+4.+4.4.+++4.4.4.4.4.4.4.+Lw) L) LwClI') wCMaL)pwt'9 C1) C!C3+Lw)IwNwNwLw)dCuN Nu 1N NNN rd rd rdrd rd rd rd rd rrd I rd CUCIN rd rd rd CUN N NU CUN N 1Nt 9 d4. U4.4. M MM4.4. ii iii 9N4.N.4 NNNNN N4.4.4.N N st' N NNNNN N N N N4NNNNNNNNNNNNNNNNNNNNNNNN C9 ')4.4.4.4.4.4.Nm Lw)C') Lw)NNNNt"NNNNt'w)C')CV)Lw) LwNNN CI~ t"C)~ )NN NLw)C))N N C')Lw)LwCr) LwLw)')L)CNC')Lw)Cr')Lw)IM 1C'CI Lw() Lw)C')N~L )LwC'NNN NN ) ) LwNN) ')Nrdfl r d d drdNN') L)C)C)C) ' ' ' 'N NNNNNNNNNNl~KI N w 01 w wA RI') C' ) C' d CA) C') wC')MUNNN NNNNMMMM NNNP) NNP) CNNNNNNuuNuNuNUNICuNININuCuiNCuNNCuCuCuNuCurdNNNCuN,Itdd'. a C MJr) CNNNNNun v iC'3 NUCCU0 .00 etI' ) rCdUrX0%0 0 nC) (V NN~U) 1)) 4Lw) flINNN~0 nit ) NNUC,0 net ('3 NN~0 3n4.C') N Nnnnnn n C) rdcunn 0 3) (0) NN~et' 000 et C Lw) C 40 0C) C dC7 ) ) ) ) CIwV) C i7 tC7 7 () )3)3) C 7(W)(V)(W)C) ) )) )C)i qt+ + ++ + ++ + ++ + ++ +NNNNN NNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNNN NNNt1NNNNNN ------N rd durdrudnd NNNNrd rdCuCUC Ck C C rd I~~NNNNNN NNNNNNNCCUC~uCNNN NNuuN~uu~~uu~rd rd rd rd rd CurdflIu u u~rd uuCU d rd rd rdu rd~ u~rd~ Cu ru uuru rd J "-5.41.4I~Nu N N N N N W+ "+ "+ "u "+ .+NN NN Cu4uufuu4"+-+uu "u""ufN N N N N N 94 "i CU "+U"+ "CuCUUWCUU W4 u W4CUCUCUCUCCU Cu-u-Cu~u~~u~u4W4 W4 -1 u -u CuCuCuu UCuCuCI uru r !-+CuNuNuNu -+NNN NUCrd rd CuVC') rd rd N~('Lw)et. LwC74.4. C1r)Cl'i)C)it NNC'InInN)IN.-i.4.4.,4.41-4.4.4.4.4I .4rd Cud rd(MC'1+4.4.4.4++4.+++++4.+++++4.++4.++4.++4.++++4.4.+++++4.4.4.+++4.++4.+4.++4.+++4.+4.4.+4.4.+4.4.+4.4.++4.++4.4.4.4.+4.4.+4.4.++++4.4.t'7et4.' 4.4.4.4.4.4.4. t ,4.4.4.4. 4.4.4.InO n nUIn ))3 nn)EXPLANATIONPRINTCHARACTER0VALUELE-1100.0000-1100. 0000-1050. 00001-1050.0000-1000.0000-1000. 0000 -950. 00002 -950. 0000 -900. 0000-900. 0000 -850. 00003 -850.0000 -800. 0000-800. 0000 -750. 00004 -750. 0000 -700. 0000-700.-0000 -650. 00005 -650. 0000 -600. 0000-600. 0000 -550. 00006 -550. 0000 -500. 0000-500. 0000 -450. 00007 -450. 0000 -400. 0000-400.0000 -350. 00008 -350. 0000 -300. 0000-300. 0000 -250. 00009 -250. 0000 -200. 0000GT -200. 0000Residual Magnetic Pseudo-Contour Map - Brunswick Quadrangle()t")SCALE IN GAMMAS- - - 4 e__ .-.- t#R* ;;J7.z4w4> m a' ~ -^ - - f - - t -- r_ .' { - 1 :5. S . r :z 5 - h- -- --- - t--o-- .l - -' :"- - - - -- - * - - -'f e . -Y. .

United States Department of Energy Grand Junction Office Report GJBX 103(81)

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