Caracterización de la sedimentación Lago Mare (Messiniense terminal) y de la transgresión del comienzo del Plioceno en la cuenca de Málaga (Cordillera Bética)

dc.contributor.authorGuerra Merchán, Antonio
dc.contributor.authorSerrano Lozano, Francisco
dc.contributor.authorGarcés Crespo, Miguel
dc.contributor.authorGofas, S.
dc.contributor.authorLópez Garrido, Ángel Carlos
dc.contributor.authorEl Kadiri, Khalil
dc.contributor.authorHlila, Rachid
dc.date.accessioned2014-06-03T10:53:00Z
dc.date.available2014-06-03T10:53:00Z
dc.date.issued2008
dc.description.abstractA stratigraphic unit deposited close to the Messinian-Pliocene boundary is newly discovered in the Malaga basin. This unit mainly consist of alluvial and lagoonal deposits. Paleontological and paleomagnetic data from these deposits and from the overlying sediments indicate that the former were formed in the latest Miocene, thus can be correlated with the so-called Lago Mare deposits. The latest Messinian and lower Pliocene deposits are separated by an erosive surface (latest-Messinian discontinuity) that is related to a relative sea-level fall previous to the earliest Pliocene general floodingen_US
dc.identifier.urihttp://hdl.handle.net/10272/8234
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherMiocene-Pliocene transitionen_US
dc.subject.otherLago Mare faciesen_US
dc.subject.otherMalaga basinen_US
dc.subject.otherBetic Cordilleraen_US
dc.subject.otherAtlantic- Mediterranean connectionen_US
dc.titleCaracterización de la sedimentación Lago Mare (Messiniense terminal) y de la transgresión del comienzo del Plioceno en la cuenca de Málaga (Cordillera Bética)en_US
dc.titleCharacterization of the Lago Mare sedimentation (latest Messinian) and the transgression of the beginning of the Pliocene in the Malaga basin (Betic Cordillera)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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