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Microfabric analysis of quartz in quartzite resisters of the «Garganta de las Pozas» ductile shear zone central part of the Gredos Massif

dc.contributor.authorDíaz Alvarado, Juan
dc.contributor.authorFernández Rodríguez, Carlos 
dc.contributor.authorDíaz Azpiroz, Manuel
dc.contributor.authorRamírez Rico, J.
dc.contributor.authorMoreno-Ventas Bravo, Ignacio 
dc.contributor.authorCastro Dorado, Antonio 
dc.date.accessioned2014-06-24T12:08:59Z
dc.date.available2014-06-24T12:08:59Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/10272/8338
dc.description.abstractThe NE-SW «Garganta de las Pozas» ductile shear zone goes along the contact between one of the granodioritic sheets mapped and the «Refugio del Rey» anatectic complex. As well as the descriptive work, it has been determined the microfabric and the lattice preferred orientation (OCP) by EBSD in a cuarcitic sample, both studies confirm a lateral dextral movement in the shear zone. The dynamic recristalization in quartz has been produced by three different mechanism: subgrain rotation, grain boundaries migration and dauphine twin, which correspond to a deformation temperature of 575ºCen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherGredos Massifen_US
dc.subject.otherShear zoneen_US
dc.subject.otherMicrofabricen_US
dc.titleAnálisis de la microfábrica del cuarzo en los resister cuarcíticos de la zona de cizalla dúctil de la Garganta de las Pozas, parte central del Macizo de Gredosen_US
dc.titleMicrofabric analysis of quartz in quartzite resisters of the «Garganta de las Pozas» ductile shear zone central part of the Gredos Massifeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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