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Study of the Crystallographic Preferred Orientation in Quartz at the Contact between the Gneisses and Metatexites-Diatexites of the Cerro Pelado Massif (Sierra de Comechingones, Argentina)

dc.contributor.authorCastellarlni, P.
dc.contributor.authorFernández Rodríguez, Carlos 
dc.contributor.authorOtamendi, Juan E.
dc.date.accessioned2014-10-27T10:51:18Z
dc.date.available2014-10-27T10:51:18Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10272/8985
dc.description.abstractThe quartz c-axis fabrics measured in the rocks of the high-grade unit of the Cerro Pelado massif (northern Sierra de Comechingones, Sierras Pampeanas, Argentina) allow to deduce a normal-sinistral sense of movement for the south-dipping shear zone separating the diatexite-metatexite domain to the north, from the gneissic terrane to the south. The crystallographic fabrics also indicate that the activity of this shear zone took place under high-T conditions. The deduced kinematics can account for the syn-metamorphic exhumation of the migmatite domainen_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.otherQuartz c-axis fabricsen_US
dc.subject.otherMigmatitesen_US
dc.subject.otherSierra de Comechingonesen_US
dc.subject.otherArgentinaen_US
dc.titleEstudio de la Orientación Cristalográfica Preferente del Cuarzo en el Contacto entre Gneises y Metatexitas - Diatexitas del Macizo Cerro Pelado (Sierra de Comechingones, Argentina)en_US
dc.titleStudy of the Crystallographic Preferred Orientation in Quartz at the Contact between the Gneisses and Metatexites-Diatexites of the Cerro Pelado Massif (Sierra de Comechingones, Argentina)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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