@article{10272/13749, year = {1995}, url = {http://hdl.handle.net/10272/13749}, abstract = {Quartz 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 -slip on prismatic and basal planes, respectively, were activated in migmatites and schists}, publisher = {Sociedad Geológica de España}, keywords = {Los Reales Nappe}, keywords = {Quartz}, keywords = {Fabric transition}, title = {Variación de la fábrica del cuarzo en el manto de Los Reales (Cordilleras Béticas)}, title = {Quartz fabric variation in the Los Reales nappe (Betic Cordillera)}, author = {García San Millán, R. S. and Tubía, José María}, }