Fenómenos de cizalla en los granitoides de la Sierra de San Vicente (Sierra de Gredos)

1. Casquet Martín, César
2. Capote del Villar, Ramón
3. Doblas Lavigne, Miguel Manuel de las

Export

Export

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Export

×

This document cannot be exported because it belongs to another portal.

Full text

lock_openFull text externo

DIALNET GOOGLE SCHOLAR lock_openOpen access editor

More publications in: Studia geologica salmanticensia

Abstract

At the east of the metamorphic outcrop of San Vicente, some granitoids with shear deformations are found. We define two zones of deformation: � A NW-Se band of sinistral shearing, at the N. � A large zone of distensive shearing, at the centre and S. These granitoids show a foliation (S planes), two foliations-partitions (Q and C2 planes) and some black mylonitic zones.

Data source: Dialnet