Magnetotelluric observations across the Juan de Fuca subduction system in the EMSLAB project

A magnetotelluric (MT)transect has been obtained near latitude 45øN from the active Juan de Fuca Spreading center, across the subduction zone and Cascades volcanic arc, and into the back arc Deschutes Basin region. This paper presents the MT data set and describes its major characteristics as they pertain to the resistivity of the subduction system. In addition, we discuss the measurement and processing procedures employed as well as important concerns in data interpretation. Broadband audiomagnetotelluric (AMT)/MT soundings( approx. 0.01-500 s period) were collected on land with considerable redundancy in site location, and from which 39 sites were selected which constrain upper crustal heterogeneity but sense also into the upper mantle. Fifteen long-period MT recordings (about 50-10,000 s) on land confirm the broadband responses in their common period range and extend the depths of exploration to hundreds of kilometers. On the Juan de Fuca plate offshore, 33 out of 39 sea floor instruments at 19 locations gave good results. Of these locations, five magnetotelluric soundings plus two additional geomagnetic variation sites, covering the period range 200-10^(5) s approximately, constitute the ocean bottom segment of our profile. The feature of the land observations which probably relates most closely to the subduction process is a peak in the impedance phase of the transverse magnetic mode around 30-50 s period. This phase anomaly, with a corresponding inflection in the apparent resistivity, is continuous eastward from the seacoast and ends abruptly at the High Cascades. It signifies an electrically conductive layer in otherwise resistive lower crust or upper mantle, with the layer conductance decreasing eastward from the coast to a minimum under the Coast Range but increasing suddenly to the east of the central Willamette Basin. The higher conductance to the east is corroborated by the vertical magnetic field transfer function whose real component shows negative values in the period range 100-1000 s over the same distance. The transverse electric mode apparent resistivity and phase on the land display a variety of three-dimensional effects which make their interpretation difficult. Conversely, both modes of the ocean floor soundings exhibit a smooth progression laterally from the coastal area to the spreading ridge, indicating that the measurements here are reflecting primarily the large-scale tectonic structures of interest and are little disturbed by small near-surface inhomogeneities. The impedance data near the ridge are strongly suggestive of a low-resistivity asthenosphere beneath resistive Juan de Fuca plate lithosphere. Approaching the coastline to the east, both impedance and vertical magnetic field responses appear increasingly affected by a thick wedge of deposited and accreted sediments and by the thinning of the seawater

WRRCTR No.10 Feasibility of Radio Sounding to the Groundwater Table in Hawaii

The reported high values of resistivity in the near surface zones in semi-arid regions on the island of Hawaii motivated research into the feasibility of using radio waves to sound the depth to the ground water table. Field tests using a 35 MHz ranging system (built in England for ice depth sounding) were made in areas of differing geology and climate, but in no instance was an echo identified as having originated from the water table. Measurements made of transmissions from within an inclined tunnel and received at the surface gave rise to a signal which may have travelled through a water saturated rock column at a velocity of 27 m/μsec while attenuated by about 3 db/m. Equipment ringing, due to antenna miss-matches, contributed to the lack of success in measuring water table echoes. However, subsequent laboratory dielectric measurements in the frequency range 10^2 to 6.2 x 10^7 Hz on representative Hawaiian rocks and soil indicate that even small amounts of moisture result in prohibitive attenuation losses. For example, in a low density basalt, the attenuation at 18 MHz is 0.26 db/m when dry, but increases to 1.66 db/m with less than 4% water by volume. In a volcanic ash soil sample, the loss increases at 18 MHz from 0.04 db/m to 1.3 db/m as the soil water content is increased from zero to 19% by volume. Electromagnetic propagation velocities decrease markedly with increasing moisture content, an effect which is most striking at low frequencies. In situ moisture conditions above the water table in the semi-arid regions in Hawaii are expected to be approximately ≥ 4% in rock and ≥ 19% in soil. Considering all factors, usable echoes at 35 MHz are consequently expected when sounding water table depths of ~˂25 m. However, frequencies as high as 0.1 MHz may prove useful in sounding depths to many hundred meters. The use of VHF (30-300 MHz) waves to probe the depths of drier environments such as possibly exist on the moon is considered feasible.U.S. Department of the Interior Grant/Contract No. 14-01-0001-1061; B-005-H

Environmental Waste Site Characterization Utilizing Aerial Photographs, Remote Sensing, And Surface Geophysics

Six different techniques were used to delineate a 40 year old trench boundary at Los Alamos National Laboratory. Data from historical aerial photographs, a magnetic gradient survey, airborne multispectral and thermal infra-red imagery, seismic refraction, DC resistivity, and total field magnetometry were utilized in this process. Each data set indicated a southern and northern edge for the trench. Average locations and 95% confidence limits for each edge were determined along a survey line perpendicular to the trench. Trench edge locations were fairly consistent among all six techniques. Results from a modeling effort performed with the total magnetic field data was the least consistent. However, each method provided unique and complementary information. The integration of all this information led to a more complete characterization of the trench boundaries and contents. I. INTRODUCTION The Los Alamos National Laboratory (LANL), located in northern New Mexico (Fig. 1), has been engag..

Origin of High Mountains in the Continents: The Southern Sierra Nevada

Active and passive seismic experiments show that the southern Sierra, despite standing 1.8 to 2.8 kilometers above its surroundings, is underlain by crust of similar seismic thickness, about 30 to 40 kilometers. Thermobarometry of xenolith suites and magnetotelluric profiles indicate that the upper mantle is eclogitic to depths of 60 kilometers beneath the western and central parts of the range, but little subcrustal lithosphere is present beneath the eastern High Sierra and adjacent Basin and Range. These and other data imply the crust of both the High Sierra and Basin and Range thinned by a factor of 2 since 20 million years ago, at odds with purported late Cenozoic regional uplift of some 2 kilometers