La aureola de contacto de Porcía-Salave ( NO de Asturias): paragénesis y condiciones termobarométricas

dc.contributor.authorRodríguez Vieítez, N.
dc.contributor.authorSuárez Hernando, Oier
dc.date.accessioned2015-02-03T11:23:30Z
dc.date.available2015-02-03T11:23:30Z
dc.date.issued2000
dc.description.abstractThe Porcia-Salave contact aureole surround the igneous complex consisting of gabbros and granodiorites emplaced in a chlorite-zone metasedimentary rocks. Andalucite-cordierite-biotite assemblages are the most common at intermediate grade. Adjacent to the intrusive contact assemblages involving combinations of cordierite, andalusite, sillimanite and K felspar; spinel and corundum appears in quartz-absent rocks. The pressure contact metamorphism estimated on minerals equilibria is 2.6-3 kbar. Application of garnet-biotite and spinel-cordierite exchange thermometry gave T > 800 °C which are consistent with equibria involving Spl+Qtz=Crd.en_US
dc.identifier.urihttp://hdl.handle.net/10272/9793
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.otherContact aureoleen_US
dc.subject.otherThermometryen_US
dc.subject.otherQuartz-absent rocksen_US
dc.subject.otherSpinelen_US
dc.subject.otherCorundunen_US
dc.titleLa aureola de contacto de Porcía-Salave ( NO de Asturias): paragénesis y condiciones termobarométricasen_US
dc.titleThe Porcía-Salave contad aureole, NW of Asturias: mineral assemblages and thermobarometryeng
dc.typejournal articleen_US
dspace.entity.typePublication

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