RT Journal Article
T1 Deformación en yesos del Triásico en el sector oriental de la Falla de Socovos (sureste de España)
T1 Deformation of Triassic gypsum in the eastern sector of the Socovos Fault (southeast Spain)
A1 Pérez Valera, Fernando
A1 Sánchez Gómez, Mario
A1 Pérez Valera, Luis Alfonso
A1 Pérez López, Alberto
AB A Triassic gypsiferous formation is juxtaposed to the Socovos Fault along its eastern portion. Here, the gypsum shows penetrative cataclastic fabrics, particularly prominent in the main fault zone. The fabrics show a profuse catalog of kinematic markers. The consistence between the kinematic criteria and the sense of the strike-slip faulting suggest that the fabrics have been generated, at least in a late stage, by tectonic strain. We propose that gypsum fabrics could help to analyze the structure in shallow tectonic environments. Testing this hypothesis would be highly useful in the Betics, were gypsum-bearing Triassic rocks crop out in extensive areas
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7853
UL http://hdl.handle.net/10272/7853
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026