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dc.contributor.authorMartínez del Olmo, W.
dc.contributor.authorLeret Verdú, G.
dc.contributor.authorSuárez Alba, J.
dc.date.accessioned2020-07-10T07:36:35Z
dc.date.available2020-07-10T07:36:35Z
dc.date.issued1986
dc.identifier.urihttp://hdl.handle.net/10272/18497
dc.description.abstractThe main structural features of the external and internal Prebetic domains allow its subdividion into three great areas that exhibit an increasing diapiric activity from NNW to SSE. The amount of diapiric structurations points to a minimum final tectonic shortening and enable us to interpret the relationships between basement and its sedimentary cover over an extense area of the Betic chaines_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.otherDiapiric structurationes_ES
dc.subject.otherBetic chaines_ES
dc.subject.otherPrebetices_ES
dc.titleLa estructuración diapírica del Sector Prebéticoes_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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