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![](./images/clear.gif) 1.- Failure modes and normal faulting in Miocene carbonate rocks, Granada Basin, Spain; implications for fluid flow units
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
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![](./images/clear.gif) 2.- Fault growth as a key control on the sedimentary architecture and depositional environments of extensional basins; the case study of the Tablate area (Granada Basin, Spain)
Societa Geologica Italiana; Rome; ITA; Italy, 2013
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![](./images/clear.gif) 3.- Inner structure and deformation mechanisms of normal faults in conglomerates and carbonate grainstones (Granada Basin, Betic Cordillera, Spain); inferences on fault permeability
Elsevier; Oxford; III; International, 2012
Fault zone structure, mechanics and evolution in nature and experiment
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![](./images/clear.gif) 4.- Mechanical stratigraphy in carbonate rocks; examples from the Maiella Mountain (central Italy) and the Granada Basin (southern Spain)
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
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![](./images/clear.gif) 5.- Stratigraphic and structural evolution of the Tablate area (Granada Basin, Spain); inferences on the possible seismic activity of the Padul Fault
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
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