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Análisis 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 Gredos

descriptionPublicationkeyboard_double_arrow_right Article 01 Jan 2007 Spain Spanish; Castilian Publisher:Sociedad Geológica de España
Authors: Díaz Alvarado, J.; Fernández, C.; Díaz Azpiroz, M.; Ramírez Rico, Joaquín; Moreno Ventas, I.; Castro, Alicia;

handle: 11441/71098 , 10261/8659 , 10272/8338

Análisis 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 Gredos

Abstract

The 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 575ºC.

Este trabajo ha sido financiado con los proyectos CGL2004-06808-CO4-01 y CGL2004-06808-CO4-02.

43ª Sesión Científica. Móstoles, Noviembre de 2007

Peer reviewed

Country
Spain
Related Organizations
Keywords

Gredos Massif, Microfabric, Shear zone, microfabric

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popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
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influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
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impulse
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