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Contact metamorphism and hydrothermalism related to the La Maladeta batholith: isotope geochemistry of C & O of carbonates

dc.contributor.authorDelgado, J.
dc.contributor.authorSoler Gil, Albert
dc.contributor.authorArcos, D.
dc.date.accessioned2017-01-25T11:01:26Z
dc.date.available2017-01-25T11:01:26Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/13159
dc.description.abstractThe isotopic composition of carbonates related to the skarn and contact metamorphic aureole of La Maladeta batholith show a broad range of variation. The whole set of obtained data can be modeled by means of an isotopic exchange between a fluid equilibrated with a magma, with an isotopic composition of ô '“O smow =8-5% o and unknow S IJCmB at Xco, < 0 . 0 2 and a Devonian limestone of 8 laO Mnw= 2 8 -29%o 8 I3Cpdi=4-5%o Volatilization processes have been observed previosly to isotopic exchangeen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCen_US
dc.subject.otherO. stable isotopesen_US
dc.subject.otherGeochemistry,en_US
dc.subject.otherSkarnen_US
dc.subject.otherHercynianen_US
dc.subject.otherPyreneesen_US
dc.titleEl metamorfismo de contacto e hidrotermalismo asociados al batolito de la Maladeta: Geoquímica isotópica de C y O en carbonatesen_US
dc.titleContact metamorphism and hydrothermalism related to the La Maladeta batholith: isotope geochemistry of C & O of carbonateseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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