@article{10272/8682,
year = {2005},
url = {http://hdl.handle.net/10272/8682},
abstract = {The Almanzora Corridor in the Betic Cordilleras is affected by brittle deformations since the Tortonian. The
analysis of fault overprinting shows a first group formed by a set of E-W dextral strike-slip faults, N-S leftlateral
strike-slip faults and NW-SE normal faults compatible with a NW-SE shortening and an associated
NE-SW extension. A second group corresponds to younger NW-SE normal faults, formed during NE-SW
oblique extension to the Corridor, with an oblate stress ellipsoid that also reactivates, in some cases,
previous faults. A more recent stress ellipsoid indicates extension, that is locally pluridirectional and reactivate
previous fault surfaces, although horizontal striations have been overprinted in the Somontín fault, associated
to a NW-SE recent shortening that is only locally registered},
publisher = {Sociedad Geológica de España},
title = {Superposición de fallas y paleoesfuerzos en el Corredor del Almanzora desde el Tortoniense a la actualidad (Cordilleras Béticas)},
title = {Fault overprinting and paleostresses in the Almanzora Corridor from the Tortonian to the Present (Betic
Cordilleras)},
author = {Pedrera Parias, Antonio and Galindo Zaldívar, Jesús and Sanz de Galdeano, Carlos and López Garrido, Ángel Carlos},
}