Evidencias geomorfológicas de actividad tectónica reciente en la falla del Camorro (Antequera)

• Cristina Reyes-Carmona ^[1] ; J.P. Galve ^[1] ; A. Jabaloy ^[1] ; P. Ruano ^[1] ; J.V. Pérez-Peña ^[1] ; G. Booth-Rea ^[1] ; J.M. Azañón ^[1]
  1. [1] Universidad de Granada

     Universidad de Granada

     Granada, España

     
• Localización: XV Reunión Nacional de Cuaternario Bizkaia Aretoa: Bilbao, 1-5 julio 2019. Libro de resúmenes, 2019, ISBN 978-84-17713-16-4, págs. 438-441
• Idioma: español
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• Resumen

  • In this paper, we define the Camorro Fault as one of the several faults in the Torcal de Antequera Massif (MTA). Such massif is located in the central sector of the Torcal Shear Zone (ZCT). The Camorro Fault was previously defined as a dextral strike-slip fault, but field observations let us propose its recent transition to a normal fault regime. The activity of the fault with this new kinematics is also corroborated by the deposit of Quaternary debris cones, as the normal fault movement would generate enough accommodation space for cones to be deposited. These facts, together with other compiled archaeological data, lead us to conclude that the Camorro Fault is an active fault.