Search results for " geoquímica"

showing 4 items of 4 documents

A highly dynamic hot hydrothermal system in the subduction environment: Geochemistry and geochronology of jadeitite and associated rocks of the Sierr…

2021

A U-Pb zircon date of ~113 Ma revealed that a variety of jadeitites and related omphacitite, chloritite and albite-rich rocks from the subduction-related Sierra del Convento block-in-serpentinite-matrix mélange (eastern Cuba) formed nearly synchronously with MORB metabasite-derived anatectic trondhjemitic liquids at high-temperature and pressure in a hot subduction environment. Field, petrologic and geochemical data indicate hydrothermal/metasomatic processes triggered by juvenile fluids likely evolved from the crystallizing hydrous trondhjemitic melts. These fluids, variably mixed with sediment-derived fluids and channelized along fractures in the supra-slab mantle, precipitated relatively…

European communitySubductionSerpentinite mélangeSubductionArchaeologyHydrothermal circulationRocas metamóficasMetasomatic transformationGeochronologySerpentinite melangeGeneral Earth and Planetary SciencesJadeititeFluid-rock interactionGeologyPetrología y GeoquímicaAmerican Journal of Science
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Environment and subsistence strategies at La Viña rock shelter and Llonin cave (Asturias, Spain) during MIS3

2020

The sites of La Viña and Llonin have an important archaeological sequence corresponding to Marine Isotope Stage 3: Mousterian, Aurignacian and Gravettian periods. La Viña is a complex rock shelter with continuous occupations, being some (basically the Mousterian and the Aurignacian in contact levels) altered by post-depositional processes as a consequence of the irregular bedrock morphology and the type of processes involved. The cave of Llonin mainly consists of occasional human/carnivores occupations during the Mousterian and the Gravettian. The current multidisciplinary research has allowed us to obtain and match several preliminary data: site formation processes, fauna and stable isotop…

Mobility010506 paleontologyArcheologygeographygeography.geographical_feature_categoryTaphonomy060102 archaeology[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistorySubsistence agriculture06 humanities and the artsEconomy15. Life on land01 natural sciencesArchaeologyHuman/Carnivore occupationsCaveWork (electrical)Taphonomy0601 history and archaeologyPaleoclimatologyRock shelterComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesPetrología y Geoquímica
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Cinq millénaires de métallurgie en montagne basque. Les apports d'une démarche intégrée alliant palynologie et géochimie isotopique du plomb

2001

Five thousand years of metallurgy in the basque mountains : the contributions of an integrated process mixing palynology and the isotopic chemistry of lead. An interdisciplinary research combining palyno- logy and lead isotopic geochemistry was performed in a peat bog of the Basque Country, in an area recognized as being an old metallurgical centre. These various analyses make it possible to reconstitute mining and metallurgical activities and to appreciate the impact on forest during last five millennia. Several phases are attested between late Neolithic and modern times (Middle Bronze age, Late Bronze age, Antiquity and finally modern time). Most of these phases are clearly related to for…

[SHS.GEO] Humanities and Social Sciences/GeographyGeography Planning and Development[SHS.GEO]Humanities and Social Sciences/GeographyMétallurgiePays Basquepalinología ; metalurgia ; geoquímica ; historia del medio ambiental ; País Vascopalynologie ; pays basque ; géochimie ; Métallurgie ; histoire de l'environnement[ SHS.GEO ] Humanities and Social Sciences/GeographyUrban StudiesPays Basque ; palynology ; geochemistry ; metallurgy ; environmental historygéochimiehistoire de l'environnementpalynologieEarth-Surface ProcessesDemography
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¿Una nueva vertiente en el Volcán Copahue?: El caso del río Colorado.

El volcán Copahue (37°51′08″S–71°10′03″O) ha sido uno de los más estudiados del cinturón volcánico Argentino-Chileno, desarrollándose numerosos trabajos desde el punto de vista geoquímico, y en particular abarcando el estudio de las aguas del sistema. Dichos trabajos se concentran en su mayoría en las nacientes del sistema volcánico hidrotermal (SVH) (Agusto et al, 2012). Sin embargo, existen varios afluentes que alimentan al rio Caviahue de los cuales no se tiene mayor información. El objetivo de este trabajo es dterminar el origen de uno de ellos, el río Colorado. Desde el flanco E del volcán emanan dos vertientes ácidas (pH 1-2,5) y calientes (35-45°C) que se unen para formar el río Agri…

volcán Copahue vertiente río Colorado geoquímica
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