Sobre la posición estratigráfica de las "Margas de Gor", Sierra de Baza, Cordillera Bética

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dc.contributor.authorMartín Pérez, J. A.
dc.contributor.authorViseras, César
dc.date.accessioned2017-08-01T09:52:53Z
dc.date.available2017-08-01T09:52:53Z
dc.date.issued1994
dc.description.abstractThe marly sediments traditionally known as "Cor Miocene" are located at the bottom of a very thick Middle Miocene detritic ensemble composed by clasts of alpujarride, malaguide and subbetic provenance. Locally they are overthrusted by Triassic Alpujarride dolostones. They are though to have been deposited In the foredeep basin related to the North-Betic Strait, located to the north of the Betic Internal Zonees_ES
dc.identifier.urihttp://hdl.handle.net/10272/14012
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherBetic Cordilleraes_ES
dc.subject.otherNorth-Betic Straites_ES
dc.subject.otherCalcareous nannoplanktones_ES
dc.subject.otherMiddle Miocenees_ES
dc.titleSobre la posición estratigráfica de las "Margas de Gor", Sierra de Baza, Cordillera Béticaes_ES
dc.titleAbout the stratigraphic position of the "Gor Marls", Sierra de Baza, Betic Cordillera, Spaineng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 15, (1993)