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Lower-Permian faulting evolution in the Pálmaces de Jadraque-Angón region (SE border of the Spanish Central System)

dc.contributor.authorFernández Rodríguez, C.
dc.date.accessioned2020-05-28T11:23:17Z
dc.date.available2020-05-28T11:23:17Z
dc.date.issued1990
dc.identifier.urihttp://hdl.handle.net/10272/18106
dc.description.abstractThe Permian basins in the easternmost part of the Spanish Central System have been ascribed to the tectonic activity that took place during the late Hercynian. The Pálmaces half-graben is mainly due to a complex interaction between the fault system of Angón, largely affecting the hercynian metamorphic rocks, and the well-known Sarteneja Faultes_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.otherFaultses_ES
dc.subject.otherLower Permianes_ES
dc.subject.otherSpanish Centra/Systemes_ES
dc.titleEvolución durante el Pérmico inferior de las fallas de la región de Pálmaces de Jadraque-Angón (borde SE del Sistema Central español)es_ES
dc.titleLower-Permian faulting evolution in the Pálmaces de Jadraque-Angón region (SE border of the Spanish Central System)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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