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Thermobarometric estimations on coronitic metagabbros from the Segovia region (Sierra de Guadarrama)

dc.contributor.authorVillaseca, Carlos
dc.contributor.authorMartín Romera, C.
dc.contributor.authorBarbero, Luis
dc.date.accessioned2014-11-17T12:00:44Z
dc.date.available2014-11-17T12:00:44Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9312
dc.description.abstractCoronitic gabbros of tholeiitic affinity croping out in the Segovia region in relation to ductile shear zones are studied in the present work. Mineral equilibria and thermobarometric calculation indicate that maximum P-T was close to 830°C and 7 kbar. Retrograde conditions of 525-650°C and 2-3.8 kbar are estimated. Maximum calculated PT conditions agree with the general clockwise metamorphic path established for this intracontinental collisional belt, which evolves from eclogitic conditions of around 775° C and 14 kb towards granulite facies conditions like the ones estimated for this metagabbrosen_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.otherMafic granulitesen_US
dc.subject.otherP-T pathsen_US
dc.subject.otherHercynian metamorphismen_US
dc.subject.otherSierra de Guadarramaen_US
dc.titleEstimaciones termobarométricas en los metagabros coroníticos de la región de Segovia (Sierra de Guadarrama)en_US
dc.titleThermobarometric estimations on coronitic metagabbros from the Segovia region (Sierra de Guadarrama)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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