OS RELEVOS CALCÁRIOS DA REGIÃO CENTRAL DO BARROCAL ALGARVIO (SUL DE PORTUGAL) - UM MODELO TECTÓNICO The limestones reliefs of the Algarve Barrocal (south Portugal) – a tectonic model

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V. Díaz del Río, P. Bárcenas, L.M. Fernández-Salas, N. López-González, D. Palomino, J.L. Rueda, O. Sánchez-Guillamón, J.T. Vázquez Grupo de Geociencias Marinas (GEMAR) Centro Oceanográfico de Málaga Instituto Español de Oceanografía Ministerio de Economía y Competitividad

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Several Mesozoic limestone elevations of E-W elongated shape rise up in the central region of the Algarve Barrocal (Portuguese southwestern margin). Tectonic geomorphology suggests that these reliefs correspond to right lateral strike-slip contractional duplexes of a large, NW-SE trending, shear zone, with a pronounced topographic expression, whose southern boundary, located southeast of the Serra de Monchique hill, is defined by the São Marcos–Quarteira Fault Zone.

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Lopes, F., Gama Pereira, L., Gomes, A., Cunha, P., Gomes, C.R., Martins, A., (2015). OS RELEVOS CALCÁRIOS DA REGIÃO CENTRAL DO BARROCAL ALGARVIO (SUL DE PORTUGAL) - UM MODELO TECTÓNICO The limestones reliefs of the Algarve Barrocal (south Portugal) – a tectonic model. Resumens sobre el VIII SIMPOSIO SOBRE EL MARGEN, Málaga, p.145-147 IBÉRICO ATLÁNTICO (MIA15).

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