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dc.contributor.authorGonzález Casado, J. M.
dc.contributor.authorCasquet Martín, César
dc.contributor.authorCaballero, J. M.
dc.contributor.authorGalindo, Carmen
dc.contributor.authorQuílez, E.
dc.contributor.authorTornos, Fernando
dc.date.accessioned2017-08-22T10:50:03Z
dc.date.available2017-08-22T10:50:03Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/14064
dc.description.abstractSeveral 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 - N W com pression. The second is a ssociated to an extensional regime, with NE-SWandE-Wextensiones_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSpanish Central Systemes_ES
dc.subject.otherFault Analysises_ES
dc.subject.otherPermian and Upper Carboniferous Tectonic Regimees_ES
dc.titleAnálisis de la fracturación asociada a las alteraciones hidrotermales de tipo Greisen y Episienita en la Sierra del Guadarramaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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