A seismic survey in the South Alboran Sea: past and present active sedimentary systems and tectonics

Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/49924

COMPARTIR / EXPORTAR:

SHARE BASE	Comparte tu historia de Acceso Abierto
Visualizar otros formatos: MARC \| Dublin Core \| RDF \| ORE \| MODS \| METS \| DIDL \| DATACITE
Refman EndNote Bibtex RefWorks Excel CSV PDF DataCite Send via email

Título:	A seismic survey in the South Alboran Sea: past and present active sedimentary systems and tectonics
Autor:	D'Acremont, E.; Gorini, Christian; Elabbassi, Mohammed; Farran, Marcel-lí CSIC; Leroy, Sylvie; Mercier de Lépinay, Bernard; Migeon, Sébastien; Poort, Jeffrey; Ammar, Abdellah; Smit, Jeroen; Do Couto, Damien; Ercilla, Gemma CSIC ORCID ; Alonso, Belén CSIC ORCID
Palabras clave:	Alboran Seismic Sedimentary Tectonic Messinian Plio-Quaternary Contourites Xauen-Tofiño
Fecha de publicación:	22-may-2012
Resumen:	Since the Tortonian, the thinned continental crust and the overlying sedimentary cover of the Alboran Sea are submitted to tectonic inversion due to the convergence between Eurasia and Africa. The past and present deformation is significant along the Moroccan margin where the MARLBORO-1 cruise in 2011, acquired 1100 km of mid-resolution seismic reflection along 20 profiles perpendicular and parallel to the margin, off Al Hoceima, to latitude 36°N. The study area located on the Xauen/Tofino banks and the South Alboran ridge off Morocco, shows signs of both past and present strong tectonic deformation, submarine landslides, and contourites EGU General Assembly 2012, Vienna, 22-27 April
URI:	http://hdl.handle.net/10261/49924
Aparece en las colecciones:	(ICM) Comunicaciones congresos