@article{10272/14066,
year = {1992},
url = {http://hdl.handle.net/10272/14066},
abstract = {Several episodes of hydrothermal activity have recently been dated in the Sierra del Guadarrama (Caballero et ai, 1992a). Stress analysis based upon the fault sets associated with 300-290 M.a. (Wlodes and greisens) and 274±6M.a. (episyenites) events, have been carried out. The first peak is related to a transtensional strike-slip tectonic regime, with S E-NW compression. The second is a ssociated to an extensional regime, with NE-SW and E-Wextension},
publisher = {Sociedad Geológica de España},
keywords = {Spanish Central System},
keywords = {Fault Analysis},
keywords = {Permian and Upper Carboniferous Tectonic Regime},
title = {Análisis de la fracturación asociada a las alteraciones hidrotermales de tipo Greisen y Episienita en la Sierra del Guadarrama},
author = {González Casado, J. M. and Casquet Martín, César and Caballero, J. M. and Galindo, Carmen and Quílez, E. and Tornos, Fernando},
}