English   español  
Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/162063
COMPARTIR / IMPACTO:
Estadísticas
logo share SHARE   Add this article to your Mendeley library MendeleyBASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:
Título

Architectures of the Moroccan continental shelf of the Alboran Sea: insights from high-resolution bathymetry and seismic data

AutorLafosse, Manfred; Gorini, Christian; Leroy, Pascal; D'Acremont, E.; Rabineau, M.; Alonso, Belén ; Ercilla, Gemma ; Ammar, Abdellah
Fecha de publicación20-abr-2016
EditorEuropean Geosciences Union
CitaciónGeophysical Research Abstracts 18: EGU2016-13736-1 (2016)
ResumenThe MARLBORO and the SARAS oceanographic surveys have explored the continental shelf in the vicinity of the transtensive Nekor basin (South Alboran Sea, Western Mediterranean) and over three submarine highs located at several tens of kilometers from the shelf. Those surveys have produced high-resolution (≤29m2/pixel) bathymetry maps. Simultaneously, seismic SPARKER and TOPAS profiles were recorded. To quantify and understand Quaternary vertical motions of this tectonically active area, we searched for morphological and sedimentary paleobathymetric or paleo-elevations markers. Shelf-edge wedges associated marine terraces and paleo-shorelines have been identified on the bathymetry and on seismic cross-sections. These features reflect the trends of long term accommodation variations. Along the Moroccan continental shelf the lateral changes of shelf-edges geometries and the spatial distribution of marine landforms (sedimentary marine terraces, sediment wave fields, marine incisions) reflect the interaction between sea level changes and spatial variations of subsidence rates. Positions of paleo-shorelines identified in the studied area have been correlated with the relative sea-level curve (Rohling et al., 2014). Several still stands or slow stands periods have been recognized between -130-125m, -100-110m and -85-80m. The astronomical forcing controls the architecture of Mediterranean continental shelves. Marine landforms distribution also reveals the way sea level changed since the LGM. The comparison with observations on other western Mediterranean margins (e.g. the Gulf of Lion, the Ionian-Calabrian shelf) allowed a first order access to vertical motion rates
DescripciónEuropean Geosciences Union General Assembly 2016 (EGU2016), 17-22 April 2016, Vienna, Austria.-- 1 page
Versión del editorhttps://meetingorganizer.copernicus.org/EGU2016/posters/22195
URIhttp://hdl.handle.net/10261/162063
Identificadoresissn: 1607-7962
Aparece en las colecciones: (ICM) Comunicaciones congresos
Ficheros en este ítem:
Fichero Descripción Tamaño Formato  
Lafosse_et_al_2016.pdf17,55 kBAdobe PDFVista previa
Visualizar/Abrir
Mostrar el registro completo
 


NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.