García San Millán, R. S.Tubía, José María2017-05-292017-05-291995http://hdl.handle.net/10272/13749Quartz 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 schistsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Los Reales NappeQuartzFabric transitionjournal articleopen access