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Study of fracturing in the southern sector of Sierra Almijara (province of Málaga)

dc.contributor.authorPérez Ramos, Isaac
dc.contributor.authorPistre, S.
dc.contributor.authorAndreo Navarro, Bartolomé
dc.contributor.authorSanz de Galdeano, Carlos
dc.description.abstractBy means of a photointerpretation study, the main fault sets have been determined in the Sierra Almijara, in the Betic Cordillera. The more frequent directions are N20-40E, N50-70E, N90-100E, N120-140E and N140-160E. They are consistent with some of the main stress fields occurred in the Betic Cordillera. The paleostresses responsible of fracturing have been inferred from regional and field data. Many of the movements of these faults occurred since de late Tortonian, during a very important uplifting of the Betic Range, up to the Quaternaryen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherBetic Cordilleraen_US
dc.subject.otherSierra Almijaraen_US
dc.titleEstudio de la fracturación en el sector meridional de Sierra Almijara (provincia de Málaga)en_US
dc.titleStudy of fracturing in the southern sector of Sierra Almijara (province of Málaga)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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