
handle: 10261/147731 , 10261/147733
The seismic experiments conducted in northern Morocco during the last decade have provided detailed information on the geometry of the crust beneath the Rif Cordillera. In the mainframe of the RIFSIS project, 2D models of velocity / depth along two 300 km-long profiles oriented NS and EW, have revealed the presence of a thickened area, with depths of Moho near 50 km under the External Rif. The crustal geometry of this area has also been investigated using passive seismic data using methods based on the analysis of receiver functions and obtaining consistent values. The origin of the thickening under the External Rif is related to the slab of Alboran, which would still be connected to the lithosphere under this area, hence causing the crustal deformation.
La financiación para este trabajo proviene del Ministerio de Economía mediante los proyectos CGL2009-09727 (RIFSIS), CSD 2006-00041 (TopoIberia), CGL2007-63889 (SIMA), CGL2008-3474 (TopoMed) y de la subvención de la Generalitat de Catalunya 2009SGR996. Hemos utilizado también datos del proyecto PICASSO, financiado por el proyecto EAR0808939 de la NSF de Estados Unidos
Peer Reviewed
Controlled source and natural seismicity data, Slab de Alboran conectado a la litosfera, Grosor cortical bajo el Rif, Datos de sismicidad natural y de fuente sísmica controlada, Crustal thickness variations beneath the Rif Cordillera, Vertical slab attached to the lithosphere beneath the Rif Cordillera
Controlled source and natural seismicity data, Slab de Alboran conectado a la litosfera, Grosor cortical bajo el Rif, Datos de sismicidad natural y de fuente sísmica controlada, Crustal thickness variations beneath the Rif Cordillera, Vertical slab attached to the lithosphere beneath the Rif Cordillera
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