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- W2071759638 abstract "Les vitesses mesurées par GPS, combinées avec les données de sismologie, ont permis d’évaluer la situation sismotectonique actuelle des différents domaines structuraux de l’arc Bético-Rifain (Maroc et Ibérie). Les mouvements sont asymétriques dans la région d’Alboran, accommodant la convergence entre l’Afrique (Nubie) et l’Eurasie. Alors que les Bétiques rattachées à l’Ibérie se déplacent vers le sud-est par rapport à l’Afrique, le Rif se subdivise en trois blocs distincts : (1) le bloc de Tanger se déplaçant vers le sud-est, (2) le bloc central du Rif se déplaçant vers le SSW et (3) le bloc oriental du Rif, avec une rotation dans le sens horaire. Les mouvements s’amortissent des nappes du Rif vers l’avant-pays. GPS velocities and seismicity across the Betic–Rif Arc structural domains (Morocco and Iberia) provide a basis to evaluate present-day seismotectonic processes between different deformation belts. The results show asymmetric movements in the complex Alboran system accommodating the convergence between the African (Nubian) and Eurasian plates. While the Betic Mountains are attached to Iberia, moving toward the southeast with respect to Africa, the Rif is divided into three blocks with distinct displacements relative to Nubia: (1) the Tangier block moving southeastward, (2) the Central Rif block moving SSW, and (3) the Oriental Rif block undergoing clockwise rotation. GPS-derived motions decrease in rate from the Rif nappes complex to the foreland." @default.
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- W2071759638 date "2008-06-01" @default.
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- W2071759638 title "Mouvements actuels des blocs tectoniques dans l’arc Bético-Rifain à partir des mesures GPS entre 1999 et 2005" @default.
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- W2071759638 doi "https://doi.org/10.1016/j.crte.2008.02.003" @default.
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