RT Journal Article
T1 Superposición de fallas y paleoesfuerzos en el Corredor del Almanzora desde el Tortoniense a la actualidad (Cordilleras Béticas)
T1 Fault overprinting and paleostresses in the Almanzora Corridor from the Tortonian to the Present (BeticCordilleras)
A1 Pedrera Parias, Antonio
A1 Galindo Zaldívar, Jesús
A1 Sanz de Galdeano, Carlos
A1 López Garrido, Ángel Carlos
AB The Almanzora Corridor in the Betic Cordilleras is affected by brittle deformations since the Tortonian. Theanalysis of fault overprinting shows a first group formed by a set of E-W dextral strike-slip faults, N-S leftlateralstrike-slip faults and NW-SE normal faults compatible with a NW-SE shortening and an associatedNE-SW extension. A second group corresponds to younger NW-SE normal faults, formed during NE-SWoblique 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 reactivateprevious fault surfaces, although horizontal striations have been overprinted in the Somontín fault, associatedto a NW-SE recent shortening that is only locally registered
PB Sociedad Geológica de España
YR 2005
FD 2005
LK http://hdl.handle.net/10272/8682
UL http://hdl.handle.net/10272/8682
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026