Large Earthquakes at the Ibero-Maghrebian Region: Basis for an EEWS |
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| Authors: | Email author" target="_blank">Elisa?BufornEmail author Agustín?Udías Carmen?Pro |
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| Institution: | 1.Dpto. de Geofísica y Meteorología, Facultad de C.C. Físicas,Universidad Complutense de Madrid,Madrid,Spain;2.Dpto. de Física, Centro Universitario de Mérida,Universidad de Extremadura,Mérida,Spain |
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| Abstract: | Large earthquakes (Mw > 6, Imax > VIII) occur at the Ibero-Maghrebian region, extending from a point (12ºW) southwest of Cape St. Vincent to Tunisia, with different characteristics depending on their location, which cause considerable damage and casualties. Seismic activity at this region is associated with the boundary between the lithospheric plates of Eurasia and Africa, which extends from the Azores Islands to Tunisia. The boundary at Cape St. Vincent, which has a clear oceanic nature in the westernmost part, experiences a transition from an oceanic to a continental boundary, with the interaction of the southern border of the Iberian Peninsula, the northern border of Africa, and the Alboran basin between them, corresponding to a wide area of deformation. Further to the east, the plate boundary recovers its oceanic nature following the northern coast of Algeria and Tunisia. The region has been divided into four zones with different seismic characteristics. From west to east, large earthquake occurrence, focal depth, total seismic moment tensor, and average seismic slip velocities for each zone along the region show the differences in seismic release of deformation. This must be taken into account in developing an EEWS for the region. |
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