3D geometry and architecture of a normal fault zone in poorly lithified sediments: A trench study on a strand of the Baza Fault, central Betic Cordillera, south Spain

Author:

Medina-Cascales Iván,Koch Leah,Cardozo Néstor,Martin-Rojas IvánORCID,Alfaro Pedro,García-Tortosa Francisco J.

Publisher

Elsevier BV

Subject

Geology

Reference86 articles.

1. A calibrated mammal scale for the Neogene of western Europe; state of the art;Agustí;Earth Sci. Rev.,2001

2. Geochemical traces of CO2 rich fluid flow along normal faults in central Italy;Agosta;Geophys. J. Int.,2008

3. Soft-sediment deformation structures induced by earthquakes (seismites) in Pliocene lacustrine deposits (Guadix- Baza basin, Central Betic Cordillera);Alfaro;Eclogae Geol. Helv.,1997

4. The Baza Fault: a major active extensional fault in the central Betic Cordillera (south Spain);Alfaro;Int. J. Earth Sci.,2008

5. The significance of giant seismites in the Plio- Pleistocene Baza palaeo-lake (S. Spain);Alfaro;Terra. Nova,2010

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