@article{10272/8805,
year = {2004},
url = {http://hdl.handle.net/10272/8805},
abstract = {By 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 Quaternary},
publisher = {Sociedad Geológica de España},
keywords = {Betic Cordillera},
keywords = {Fracturing},
keywords = {Paleostresses},
keywords = {Sierra Almijara},
title = {Estudio de la fracturación en el sector meridional de Sierra Almijara (provincia de Málaga)},
title = {Study of fracturing in the southern sector of Sierra Almijara (province of Málaga)},
author = {Pérez Ramos, Isaac and Pistre, S. and Andreo Navarro, Bartolomé and Sanz de Galdeano, Carlos},
}