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Quartz fabric variation in the Los Reales nappe (Betic Cordillera)

dc.contributor.authorGarcía San Millán, R. S.
dc.contributor.authorTubía, José María
dc.date.accessioned2017-05-29T12:25:59Z
dc.date.available2017-05-29T12:25:59Z
dc.date.issued1995
dc.identifier.urihttp://hdl.handle.net/10272/13749
dc.description.abstractQuartz fabrics from tectonites belonging to the metamorphic sequence of the Los Reales nappe, in the Betic cordillera (SE Spain), provide a fabric zoning which mainly reflects different temperature conditions during plastic deformation. In XZ section the most representative diagrams of quartz c-axes range from pronounced maxima near the stretching lineation in granulitic samples, through maxima over the Y-axes in migmatites, to maxima at high angles to the foliation in the schists. This fabric variation. suggests that [c]-slip was dominant in granulitic rocks whereas <a>-slip on prismatic and basal planes, respectively, were activated in migmatites and schistsen_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.otherLos Reales Nappeen_US
dc.subject.otherQuartzen_US
dc.subject.otherFabric transitionen_US
dc.titleVariación de la fábrica del cuarzo en el manto de Los Reales (Cordilleras Béticas)en_US
dc.titleQuartz fabric variation in the Los Reales nappe (Betic Cordillera)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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