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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.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-NW compression. The second is a ssociated to an extensional regime, with NE-SW and E-Wextensiones_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
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

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Atribución-NoComercial-SinDerivadas 3.0 España
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