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Strike-slip faults in the south Haouz (Calcareous Dorsal, Internal Rif, N of Tetouan, Maroc). Comparison with the Betics (Spain)

dc.contributor.authorEl Adraoui, A.
dc.contributor.authorAït Brahim, L.
dc.contributor.authorSanz de Galdeano, Carlos
dc.description.abstractDifferent sets of strike-slip faults of the Haouz Mountains (from Tetouan to the strait of Gibraltar) deform the tectonic slices of the Calcareous Dorsal there present. In this paper we study those faults at the southern part of the Haouz. Three fault formation stages can be distinguished and correspond to the progressive s1 rotation during the Neogene from a near E-W position to approximately N-S, in a progressive anticlockwise rotation. The faults and other related structures are compared with similar ones existing in the Betic Cordillera, in equivalent areas of the arc of Gibraltaren_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherStrike-slip faulten_US
dc.subject.otherBetic-Rifian Internal Zoneen_US
dc.subject.otherCalcareous Dorsalen_US
dc.subject.otherHaouz Rangeen_US
dc.titleFallas de salto en dirección en el Haouz meridional (Complejo de la Dorsal, Rif interno, N de Tetuán, Marruecos). Comparación con las Béticas (España)en_US
dc.titleStrike-slip faults in the south Haouz (Calcareous Dorsal, Internal Rif, N of Tetouan, Maroc). Comparison with the Betics (Spain)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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