Fallas de salto en dirección en el Haouz meridional (Complejo de la Dorsal, Rif interno, N de Tetuán, Marruecos). Comparación con las Béticas (España)

Abstract

Different 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 Gibraltar