La dolomitización de la base de la Formación «Dolomías de Landete» en la Sierra de Espadan, (Castellón): datos de geoquímica isotópica (C, O y Sr) e inclusiones fluidas

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dc.contributor.authorTritlla, J.
dc.contributor.authorCardellach, Esteve
dc.date.accessioned2016-06-14T12:21:20Z
dc.date.available2016-06-14T12:21:20Z
dc.date.issued1996
dc.description.abstractThe dolomitization affecting the basal facies of the «Landete Dolostone» Formation in Sierra de Espadán (Castellón Province, Iberian Ranges) has been studied using fluid inclusions, stable (C and O) and radiogenic (Sr) isotopes. Two different processes have been found: (1) a pervasive epigenetic dolomitization originated by mixing of two different fluids of contrasted composition, and (2) the generation of «zebra»-llke rhythmic textures formed from hot (215 °C), high salinity (20-24 wt% eq NaCI) connate fluids equilibrated with the enclosing dolostone ( 8 18O H2O= + 13.0%o). A link between this high temperature event and the presence of a Hg deposit in the area is proposeden_US
dc.identifier.urihttp://hdl.handle.net/10272/12340
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.otherDolostoneen_US
dc.subject.otherDolomitizationen_US
dc.subject.otherZebra texturesen_US
dc.subject.otherFluid inclusionsen_US
dc.subject.otherStable isotopesen_US
dc.subject.otherStrontium isotopesen_US
dc.subject.otherTriassicen_US
dc.titleLa dolomitización de la base de la Formación «Dolomías de Landete» en la Sierra de Espadan, (Castellón): datos de geoquímica isotópica (C, O y Sr) e inclusiones fluidasen_US
dc.titleDolomitization at the base of the «Landete Dolostones» formation in Sierra de Espadán (Castellón province): isotopic geochemistry (C, O and Sr) and fluid inclusion dataeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-3, (1996)