@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 <a>-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},
}