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dc.contributor.authorGarcía Dueñas, V.
dc.contributor.authorMartínez Martínez, J. M.
dc.contributor.authorNavarro Villa, F.
dc.date.accessioned2020-07-10T07:49:47Z
dc.date.available2020-07-10T07:49:47Z
dc.date.issued1986
dc.identifier.urihttp://hdl.handle.net/10272/18499
dc.description.abstractThe Torres Cartas Fault Zone is a large low-angle extensional structure, strongly thinning the Nevado-Filabride and Alpujarride nappes. These nappe complexes form the basement of the Alboran sea southwest Sierra Alhamilla. The fault zone, being already probably active in Burdigalian times, was folded during the Upper Miocenees_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.otherExtensional structurees_ES
dc.subject.otherNappeses_ES
dc.subject.otherBetic Cordillerases_ES
dc.titleLa zona de falla de Torres Cartas, conjunto de fallas normales de bajo ángulo entre Nevado-Filábrides y Alpujárrides (Sierra Alhamilla, Béticas Orientales)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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