Geoquímica de los fluidos asociados a estructuras filonianas mesozoicas del anticlinal de Talayuelas (Cordillera Ibérica, Cuenca)

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dc.contributor.authorTritlla, J.
dc.contributor.authorCardellach, Esteve
dc.contributor.authorHuerta, J.
dc.date.accessioned2017-02-10T12:12:51Z
dc.date.available2017-02-10T12:12:51Z
dc.date.issued1996
dc.description.abstractIn the Talayuelas anticline (Cuenca province, Iberian Ranges) many quartz-siderite and barite ± quartz veins associated to Mesozoic faulting are found. They reflect an intense hydrothermal activity dominated by upwelling hot fluids of ultimate surficial origin (150 to 160 °C and up to 25% NaCI eq. salinity) that mixed with colder, less saline, descending solutions. Barite sulfate is related to the leaching of evaporites of Triassic to Jurassic age. The fluid circulation was probably enhanced by the high geothermal gradient related to the graben stage during the development of the Iberian rift.en_US
dc.identifier.urihttp://hdl.handle.net/10272/13273
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherIberian Rangesen_US
dc.subject.otherHydrothermal fluidsen_US
dc.subject.otherStable isotopesen_US
dc.subject.otherFluid inclusionsen_US
dc.subject.otherBariteen_US
dc.subject.otherMesozoicen_US
dc.titleGeoquímica de los fluidos asociados a estructuras filonianas mesozoicas del anticlinal de Talayuelas (Cordillera Ibérica, Cuenca)en_US
dc.titleGeochemistry of fluids associated to Mesozoic veins of the Talayuelas anticline (Cuenca, Iberian Ranges)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-7, (1996)