Análisis de la fracturación asociada a las alteraciones hidrotermales de tipo Greisen y Episienita en la Sierra del Guadarrama

dc.contributor.author	González Casado, J. M.
dc.contributor.author	Casquet Martín, César
dc.contributor.author	Caballero, J. M.
dc.contributor.author	Galindo, Carmen
dc.contributor.author	Quílez, E.
dc.contributor.author	Tornos, Fernando
dc.date.accessioned	2017-08-22T11:24:40Z
dc.date.available	2017-08-22T11:24:40Z
dc.date.issued	1992
dc.identifier.uri	http://hdl.handle.net/10272/14066
dc.description.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	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Spanish Central System	es_ES
dc.subject.other	Fault Analysis	es_ES
dc.subject.other	Permian and Upper Carboniferous Tectonic Regime	es_ES
dc.title	Análisis de la fracturación asociada a las alteraciones hidrotermales de tipo Greisen y Episienita en la Sierra del Guadarrama	es_ES
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

dc.contributor.author	González Casado, J. M.
dc.contributor.author	Casquet Martín, César
dc.contributor.author	Caballero, J. M.
dc.contributor.author	Galindo, Carmen
dc.contributor.author	Quílez, E.
dc.contributor.author	Tornos, Fernando
dc.date.accessioned	2017-08-22T11:24:40Z
dc.date.available	2017-08-22T11:24:40Z
dc.date.issued	1992
dc.identifier.uri	http://hdl.handle.net/10272/14066
dc.description.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	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Spanish Central System	es_ES
dc.subject.other	Fault Analysis	es_ES
dc.subject.other	Permian and Upper Carboniferous Tectonic Regime	es_ES
dc.title	Análisis de la fracturación asociada a las alteraciones hidrotermales de tipo Greisen y Episienita en la Sierra del Guadarrama	es_ES
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

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