RT Journal Article
T1 Caracterización de la sedimentación Lago Mare (Messiniense terminal) y de la transgresión del comienzo del Plioceno en la cuenca de Málaga (Cordillera Bética)
T1 Characterization of the Lago Mare sedimentation (latest Messinian) and the transgression of the beginning of thePliocene in the Malaga basin (Betic Cordillera)
A1 Guerra Merchán, Antonio
A1 Serrano Lozano, Francisco
A1 Garcés Crespo, Miguel
A1 Gofas, S.
A1 López Garrido, Ángel Carlos
A1 El Kadiri, Khalil
A1 Hlila, Rachid
AB A stratigraphic unit deposited close to the Messinian-Pliocene boundary is newly discovered in the Malagabasin. This unit mainly consist of alluvial and lagoonal deposits. Paleontological and paleomagnetic datafrom these deposits and from the overlying sediments indicate that the former were formed in the latestMiocene, thus can be correlated with the so-called Lago Mare deposits. The latest Messinian and lowerPliocene deposits are separated by an erosive surface (latest-Messinian discontinuity) that is related to arelative sea-level fall previous to the earliest Pliocene general flooding
YR 2008
FD 2008
LK http://hdl.handle.net/10272/8234
UL http://hdl.handle.net/10272/8234
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026