181 research outputs found
Comparative fluid inclusion studies of the San MartĂn skarn (Mexico) and the epithermal Comstock Lode (USA) and Pachuca-Real del Monte (Mexico) deposits
San MartĂn (Mexico), Pachuca-Real del Monte (MĂ©xico) y Comstock Lode (USA) son depĂłsitos de metales base y plata emplazados en rocas volcanosedimentarias del cretĂĄceo y Terciario. El primero es un depĂłsito del tipo skarn mientras que el segundo y tercero son del tipo epitermal. Un estudio de inclusiones fluidas en cuarzo, esfalerita y fluorita fue desarrollado para caracterizar las soluciones mineralizantes las cuales presentan diferentes composiciones y temperaturas. Las temperaturas de homogenizaciĂłn y salinidad de los fluidos presentes en las muestras de cuarzo y fluorita de San MartĂn varĂan entre 300 y 320 °C y 5.0 y 40 % eq. peso NaCl con base en la Tmice and TNaCl. La Halita como mineral hijo es frecuente en las muestras de cuarzo y fluorita. Sinembargo, en los otros distritos los valores en esfalerita (Pachuca-Real) y cuarzo (Comstock) son relativamente mas bajos: 265 °C y 3.4 % eq. peso NaCl y 251 °C y 0.3 % eq. peso NaCl respectivamente. Mediciones de un cristal de cuarzo zonado evidencian una evoluciĂłn de los fluidos durante las fases de mineralizaciĂłn en Comstock Lode. En este fueron observadas temperaturas y salinidades de 249 °C y 0.6 % eq peso NaCl en el nĂșcleo y 245 °C y 0.1 % eq wt. NaCl hacia el borde. La salinidad y temperatura de los fluidos hidrotermales parece ser factores importantes que influyen en la precipitaciĂłn mineral. En general estos depositos se caracterizan por temperaturas <350 °C y salinidades entre 0.0 to 40 % en. peso de NaCl. Las presiones y profundidades estimadas varĂan entre 41 y 103 bars y los 472 y 1400 metros.The San Martin (Mexico), Pachuca-Real del Monte (Mexico) and Comstock Lode (USA) are base-metal and silver deposits within Cretaceous to Tertiary volcano-sedimentary host rocks. The first is a skarn type deposit whilst the second and third are epithermal vein-type deposits. A fluid inclusion study of quartz, sphalerite and fluorite was undertaken to characterize mineralizing solutions which have different compositions and temperatures. Microthermometric measurements were made based on the recognition of changes of twophase liquid-rich, two-phase vapor-rich and multiphase (NaCl) inclusions during heating and freezing experiments. Homogenization temperatures and salinities of fluid inclusions in quartz and fluorite from San Martin range from 300 to 320 °C and 5.0 to 40 eq. wt. % NaCl based on Tmice and TNaCl. Halite as a daughter mineral is often present in quartz and fluorite. However in the other districts, the Th and salinity values in sphalerite (Pachuca-Real) and quartz (Comstock) are lower: 265 °C and 3.4 % eq. wt. NaCl and 251 °C and 0.3 eq. wt. % NaCl respectively. Data from a single zoned quartz crystal provides evidence of fluid evolution at the Comstock Lode. Temperatures and salinities observed were 249 °C and 0.6 eq wt % NaCl at the core and 245 °C and 0.1 eq wt % NaCl at the rim. The salinity and temperature of the hydrothermal brines seems to be an important factor in explaining the precipitation of the ore minerals. These deposits are characterized by temperatures <350 °C and salinities from 0.2 to 4.93 wt % eq. NaCl. Estimated pressures and depths range from 41 to 103 bars and 472 to 1394 meters
Comparative fluid inclusion studies of the San MartĂn skarn (Mexico) and the epithermal Comstock Lode (USA) and Pachuca-Real del Monte (Mexico) deposits
San MartĂn (Mexico), Pachuca-Real del Monte (MĂ©xico) y Comstock Lode (USA) son depĂłsitos de metales base y plata emplazados en rocas volcanosedimentarias del cretĂĄceo y Terciario. El primero es un depĂłsito del tipo skarn mientras que el segundo y tercero son del tipo epitermal. Un estudio de inclusiones fluidas en cuarzo, esfalerita y fluorita fue desarrollado para caracterizar las soluciones mineralizantes las cuales presentan diferentes composiciones y temperaturas. Las temperaturas de homogenizaciĂłn y salinidad de los fluidos presentes en las muestras de cuarzo y fluorita de San MartĂn varĂan entre 300 y 320 °C y 5.0 y 40 % eq. peso NaCl con base en la Tmice and TNaCl. La Halita como mineral hijo es frecuente en las muestras de cuarzo y fluorita. Sinembargo, en los otros distritos los valores en esfalerita (Pachuca-Real) y cuarzo (Comstock) son relativamente mas bajos: 265 °C y 3.4 % eq. peso NaCl y 251 °C y 0.3 % eq. peso NaCl respectivamente. Mediciones de un cristal de cuarzo zonado evidencian una evoluciĂłn de los fluidos durante las fases de mineralizaciĂłn en Comstock Lode. En este fueron observadas temperaturas y salinidades de 249 °C y 0.6 % eq peso NaCl en el nĂșcleo y 245 °C y 0.1 % eq wt. NaCl hacia el borde. La salinidad y temperatura de los fluidos hidrotermales parece ser factores importantes que influyen en la precipitaciĂłn mineral. En general estos depositos se caracterizan por temperaturas <350 °C y salinidades entre 0.0 to 40 % en. peso de NaCl. Las presiones y profundidades estimadas varĂan entre 41 y 103 bars y los 472 y 1400 metros.The San Martin (Mexico), Pachuca-Real del Monte (Mexico) and Comstock Lode (USA) are base-metal and silver deposits within Cretaceous to Tertiary volcano-sedimentary host rocks. The first is a skarn type deposit whilst the second and third are epithermal vein-type deposits. A fluid inclusion study of quartz, sphalerite and fluorite was undertaken to characterize mineralizing solutions which have different compositions and temperatures. Microthermometric measurements were made based on the recognition of changes of twophase liquid-rich, two-phase vapor-rich and multiphase (NaCl) inclusions during heating and freezing experiments. Homogenization temperatures and salinities of fluid inclusions in quartz and fluorite from San Martin range from 300 to 320 °C and 5.0 to 40 eq. wt. % NaCl based on Tmice and TNaCl. Halite as a daughter mineral is often present in quartz and fluorite. However in the other districts, the Th and salinity values in sphalerite (Pachuca-Real) and quartz (Comstock) are lower: 265 °C and 3.4 % eq. wt. NaCl and 251 °C and 0.3 eq. wt. % NaCl respectively. Data from a single zoned quartz crystal provides evidence of fluid evolution at the Comstock Lode. Temperatures and salinities observed were 249 °C and 0.6 eq wt % NaCl at the core and 245 °C and 0.1 eq wt % NaCl at the rim. The salinity and temperature of the hydrothermal brines seems to be an important factor in explaining the precipitation of the ore minerals. These deposits are characterized by temperatures <350 °C and salinities from 0.2 to 4.93 wt % eq. NaCl. Estimated pressures and depths range from 41 to 103 bars and 472 to 1394 meters
VOLUMEN 25, NĂMERO 40 (2003)
TERMOCRONOLOGĂA K-Ar EN ILLITAS: ASPECTOS METODOLĂGICOS. Mantilla Figueroa, L. C.CINĂTICA DE LA NUCLEACIĂN Y EL CRECIMIENTO DEL GRANATE EN LAS ROCAS METAPELĂTICAS DE LA FORMACIĂN SILGARĂ, REGIĂN SUROCCIDENTAL DEL MACIZO DE SANTANDER. RĂos Reyes, C., GĂ©lvez Llanes, J., MĂĄrquez Romero, R. y Castellanos AlarcĂłn, O.INTRODUCCIĂN A LA GEOLOGĂA DEL SECTOR VĂLEZâBOLĂVARâGUAVATĂ (DPTO. DE SANTANDER, COLOMBIA) Y SU IMPORTANCIA PARA LA EXPLORACIĂN DE DEPĂSITOSHIDROTERMALES. Mantilla Figueroa, L. C.; Cruz G. L. E.; Colegial G. J. D.RECOGNITION OF ANCIENT SHOREFACE DEPOSITS. FACIES, FACIES SUCESSIONS, AND ASSOCIATIONS. AN EXAMPLE FROM THE CRETACEOUS GALLUP CLASTIC WEDGE, NEW MĂXICO. Ălvarez Bastos, MNUEVAS EVIDENCIAS ACERCA DE LA PRESENCIA DE UNA BANDA DE CIZALLAMIENTO EN LA SECUENCIA METAPELĂTICA DE LA FORMACIĂN SILGARĂ, SECTOR ARATOCA-PESCADERO (REGION SUROCCIDENTAL DEL MACIZO DE SANTANDER). Mantilla Figueroa, L. C.; RĂos Reyes, C. A.; GĂ©lvez Llanes, J. R.; MĂĄrquez Romero, R. E.; Ordóñez CalderĂłn, J. C.; Cepeda Espitia, S.LOS DELIRIOS: UN YACIMIENTO HIDROTERMAL DE ORO Y PLATA EN LA REGIĂN DE VETAS, SANTANDER (COLOMBIA). GarcĂa RamĂrez, C. A., Uribe Portilla, E.MINERALOGĂA, GEOQUĂMICA Y ALGUNOS ASPECTOS GENĂTICOS DE LA MINA EL DIAMANTE - NARIĂO (COLOMBIA). Molano, J.C. and Shimazaki, H.COMPARATIVE FLUID INCLUSION STUDIES OF THE SAN MARTĂN SKARN (MĂXICO) AND THE EPITHERMAL COMSTOCK LODE (USA) AND PACHUCA-REAL DEL MONTE (MĂXICO) DEPOSITS. Campos Ălvarez, N. O
VOLUMEN 25, NĂMERO 40 (2003)
TERMOCRONOLOGĂA K-Ar EN ILLITAS: ASPECTOS METODOLĂGICOS. Mantilla Figueroa, L. C.CINĂTICA DE LA NUCLEACIĂN Y EL CRECIMIENTO DEL GRANATE EN LAS ROCAS METAPELĂTICAS DE LA FORMACIĂN SILGARĂ, REGIĂN SUROCCIDENTAL DEL MACIZO DE SANTANDER. RĂos Reyes, C., GĂ©lvez Llanes, J., MĂĄrquez Romero, R. y Castellanos AlarcĂłn, O.INTRODUCCIĂN A LA GEOLOGĂA DEL SECTOR VĂLEZâBOLĂVARâGUAVATĂ (DPTO. DE SANTANDER, COLOMBIA) Y SU IMPORTANCIA PARA LA EXPLORACIĂN DE DEPĂSITOSHIDROTERMALES. Mantilla Figueroa, L. C.; Cruz G. L. E.; Colegial G. J. D.RECOGNITION OF ANCIENT SHOREFACE DEPOSITS. FACIES, FACIES SUCESSIONS, AND ASSOCIATIONS. AN EXAMPLE FROM THE CRETACEOUS GALLUP CLASTIC WEDGE, NEW MĂXICO. Ălvarez Bastos, MNUEVAS EVIDENCIAS ACERCA DE LA PRESENCIA DE UNA BANDA DE CIZALLAMIENTO EN LA SECUENCIA METAPELĂTICA DE LA FORMACIĂN SILGARĂ, SECTOR ARATOCA-PESCADERO (REGION SUROCCIDENTAL DEL MACIZO DE SANTANDER). Mantilla Figueroa, L. C.; RĂos Reyes, C. A.; GĂ©lvez Llanes, J. R.; MĂĄrquez Romero, R. E.; Ordóñez CalderĂłn, J. C.; Cepeda Espitia, S.LOS DELIRIOS: UN YACIMIENTO HIDROTERMAL DE ORO Y PLATA EN LA REGIĂN DE VETAS, SANTANDER (COLOMBIA). GarcĂa RamĂrez, C. A., Uribe Portilla, E.MINERALOGĂA, GEOQUĂMICA Y ALGUNOS ASPECTOS GENĂTICOS DE LA MINA EL DIAMANTE - NARIĂO (COLOMBIA). Molano, J.C. and Shimazaki, H.COMPARATIVE FLUID INCLUSION STUDIES OF THE SAN MARTĂN SKARN (MĂXICO) AND THE EPITHERMAL COMSTOCK LODE (USA) AND PACHUCA-REAL DEL MONTE (MĂXICO) DEPOSITS. Campos Ălvarez, N. O
VOLUMEN 22, NĂMERO 37 (2000)
ANĂLISIS DE VARIABLES MORFOMĂTRICAS DE toxaster roulini agassiz (Echinoides: toxasteriidae) DE LA FORMACIĂN ROSA BLANCA, MUNICIPIO DE ZAPATOCA (SANTANDER, COLOMBIA). Cruz Guevara, L. E.; Jerez Jaimes, J. H., NarvĂĄez Parra, E. X.; Franco Blanco, R. A.COMPOSICIĂN QUĂMICA Y MINERALOGĂA DE LAS BIOTITAS METAMĂRFICAS DEL SECTOR CENTRAL DEL MACIZO DE SANTANDER, COLOMBIA. GarcĂa RamĂrez, C. A.; Campos Ălvarez, N. O.BRECHAS DE ATRICIĂN Y MINERALIZACIONES AURĂFERAS EN LAS MINAS DE MIRAFLORES (QUINCHĂA, RISARALDA) Y SU RELACIĂN CON UN CUERPO TIPO âBRECHA - PIPEâ. Carrillo Lombana, V. M.CRITERIOS PARA LA CLASIFICACIĂN Y DESCRIPCIĂN DE MOVIMIENTOS EN MASA. Vargas Cuervo, G.ANOMALĂAS GEOBOTĂNICAS ESPECTRALES ASOCIADAS CON LOS CAMBIOS EN LITOLOGĂA: SU USO PARA LA CARTOGRAFĂA GEOLĂGICA DE ROCAS ULTRABĂSICAS, EN TERRENOS TOTALMENTE VEGETADOS DE LA COSTA PACĂFICA COLOMBIANA. Villegas, V. H
VOLUMEN 22, NĂMERO 37 (2000)
ANĂLISIS DE VARIABLES MORFOMĂTRICAS DE toxaster roulini agassiz (Echinoides: toxasteriidae) DE LA FORMACIĂN ROSA BLANCA, MUNICIPIO DE ZAPATOCA (SANTANDER, COLOMBIA). Cruz Guevara, L. E.; Jerez Jaimes, J. H., NarvĂĄez Parra, E. X.; Franco Blanco, R. A.COMPOSICIĂN QUĂMICA Y MINERALOGĂA DE LAS BIOTITAS METAMĂRFICAS DEL SECTOR CENTRAL DEL MACIZO DE SANTANDER, COLOMBIA. GarcĂa RamĂrez, C. A.; Campos Ălvarez, N. O.BRECHAS DE ATRICIĂN Y MINERALIZACIONES AURĂFERAS EN LAS MINAS DE MIRAFLORES (QUINCHĂA, RISARALDA) Y SU RELACIĂN CON UN CUERPO TIPO âBRECHA - PIPEâ. Carrillo Lombana, V. M.CRITERIOS PARA LA CLASIFICACIĂN Y DESCRIPCIĂN DE MOVIMIENTOS EN MASA. Vargas Cuervo, G.ANOMALĂAS GEOBOTĂNICAS ESPECTRALES ASOCIADAS CON LOS CAMBIOS EN LITOLOGĂA: SU USO PARA LA CARTOGRAFĂA GEOLĂGICA DE ROCAS ULTRABĂSICAS, EN TERRENOS TOTALMENTE VEGETADOS DE LA COSTA PACĂFICA COLOMBIANA. Villegas, V. H
Influence of the Temperature and the Genotype of the HSP90AA1 Gene over Sperm Chromatin Stability in Manchega Rams
The present study addresses the effect of heat stress on males' reproduction ability. For that, we have evaluated the sperm DNA fragmentation (DFI) by SCSA of ejaculates incubated at 37°C during 0, 24 and 48 hours after its collection, as a way to mimic the temperature circumstances to which spermatozoa will be subject to in the ewe uterus. The effects of temperature and temperature-humidity index (THI) from day 60 prior collection to the date of semen collection on DFI were examined. To better understand the causes determining the sensitivity of spermatozoa to heat, this study was conducted in 60 males with alternative genotypes for the SNP G/Câ660 of the HSP90AA1 promoter, which encode for the Hsp90α protein. The Hsp90α protein predominates in the brain and testis, and its role in spermatogenesis has been described in several species. Ridge regression analyses showed that days 29 to 35 and 7 to 14 before sperm collection (bsc) were the most critical regarding the effect of heat stress over DFI values. Mixed model analyses revealed that DFI increases over a threshold of 30°C for maximum temperature and 22 for THI at days 29 to 35 and 7 to 14 bsc only in animals carrying the GGâ660 genotype. The period 29â35 bsc coincide with the meiosis I process for which the effect of the Hsp90α has been described in mice. The period 7â14 bsc may correspond with later stages of the meiosis II and early stages of epididymal maturation in which the replacement of histones by protamines occurs. Because of GGâ660 genotype has been associated to lower levels of HSP90AA1 expression, suboptimal amounts of HSP90AA1 mRNA in GGâ660 animals under heat stress conditions make spermatozoa DNA more susceptible to be fragmented. Thus, selecting against the GGâ660 genotype could decrease the DNA fragmentation and spermatozoa thermal susceptibility in the heat season, and its putative subsequent fertility gainsPublishe
EPIdemiology of Surgery-Associated Acute Kidney Injury (EPIS-AKI) : Study protocol for a multicentre, observational trial
More than 300 million surgical procedures are performed each year. Acute kidney injury (AKI) is a common complication after major surgery and is associated with adverse short-term and long-term outcomes. However, there is a large variation in the incidence of reported AKI rates. The establishment of an accurate epidemiology of surgery-associated AKI is important for healthcare policy, quality initiatives, clinical trials, as well as for improving guidelines. The objective of the Epidemiology of Surgery-associated Acute Kidney Injury (EPIS-AKI) trial is to prospectively evaluate the epidemiology of AKI after major surgery using the latest Kidney Disease: Improving Global Outcomes (KDIGO) consensus definition of AKI. EPIS-AKI is an international prospective, observational, multicentre cohort study including 10 000 patients undergoing major surgery who are subsequently admitted to the ICU or a similar high dependency unit. The primary endpoint is the incidence of AKI within 72 hours after surgery according to the KDIGO criteria. Secondary endpoints include use of renal replacement therapy (RRT), mortality during ICU and hospital stay, length of ICU and hospital stay and major adverse kidney events (combined endpoint consisting of persistent renal dysfunction, RRT and mortality) at day 90. Further, we will evaluate preoperative and intraoperative risk factors affecting the incidence of postoperative AKI. In an add-on analysis, we will assess urinary biomarkers for early detection of AKI. EPIS-AKI has been approved by the leading Ethics Committee of the Medical Council North Rhine-Westphalia, of the Westphalian Wilhelms-University MĂŒnster and the corresponding Ethics Committee at each participating site. Results will be disseminated widely and published in peer-reviewed journals, presented at conferences and used to design further AKI-related trials. Trial registration number NCT04165369
Gaia Focused Product Release: Radial velocity time series of long-period variables
The third Gaia Data Release (DR3) provided photometric time series of more
than 2 million long-period variable (LPV) candidates. Anticipating the
publication of full radial-velocity (RV) in DR4, this Focused Product Release
(FPR) provides RV time series for a selection of LPVs with high-quality
observations. We describe the production and content of the Gaia catalog of LPV
RV time series, and the methods used to compute variability parameters
published in the Gaia FPR. Starting from the DR3 LPVs catalog, we applied
filters to construct a sample of sources with high-quality RV measurements. We
modeled their RV and photometric time series to derive their periods and
amplitudes, and further refined the sample by requiring compatibility between
the RV period and at least one of the , , or
photometric periods. The catalog includes RV time series and variability
parameters for 9\,614 sources in the magnitude range , including a flagged top-quality subsample of 6\,093 stars
whose RV periods are fully compatible with the values derived from the ,
, and photometric time series. The RV time series
contain a mean of 24 measurements per source taken unevenly over a duration of
about three years. We identify the great most sources (88%) as genuine LPVs,
with about half of them showing a pulsation period and the other half
displaying a long secondary period. The remaining 12% consists of candidate
ellipsoidal binaries. Quality checks against RVs available in the literature
show excellent agreement. We provide illustrative examples and cautionary
remarks. The publication of RV time series for almost 10\,000 LPVs constitutes,
by far, the largest such database available to date in the literature. The
availability of simultaneous photometric measurements gives a unique added
value to the Gaia catalog (abridged)Comment: 36 pages, 38 figure
New insights into the genetic etiology of Alzheimer's disease and related dementias.
Characterization of the genetic landscape of Alzheimer's disease (AD) and related dementias (ADD) provides a unique opportunity for a better understanding of the associated pathophysiological processes. We performed a two-stage genome-wide association study totaling 111,326 clinically diagnosed/'proxy' AD cases and 677,663 controls. We found 75 risk loci, of which 42 were new at the time of analysis. Pathway enrichment analyses confirmed the involvement of amyloid/tau pathways and highlighted microglia implication. Gene prioritization in the new loci identified 31 genes that were suggestive of new genetically associated processes, including the tumor necrosis factor alpha pathway through the linear ubiquitin chain assembly complex. We also built a new genetic risk score associated with the risk of future AD/dementia or progression from mild cognitive impairment to AD/dementia. The improvement in prediction led to a 1.6- to 1.9-fold increase in AD risk from the lowest to the highest decile, in addition to effects of age and the APOE Δ4 allele
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