Precisiones sobre la cinemática y edad de la falla del Río de la Miel (Maro, Málaga).

1. Pérez Ramos, Isaac
2. Sanz de Galdeano Equiza, Carlos
3. Andreo Navarro, Bartolomé
4. Pistre, S.

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lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Otras publicaciones en: Geogaceta

Resumen

The Río de la Miel fault shows a complex movement history. Three main displacement stages have been distinguished from the microtectonic analysis. The first stage was a dextral strike-slip rnovement whose o was almost horizontal with a NNW-SSE direction. The second stage was a normal movement with o situated in the vertical. Finally in the third stage o had a low dipping angle and a NNE-SSW direction. The vertical displacement of the fault reach several hundreds of metres, probably more than 500 m. This fault has been active at least during the lower Pliocene.

Fuente de los datos: Dialnet