RT Journal Article
T1 Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
T1 Extensional structures in the Alpujarride materials of the East of Malaga (Sierra Tejeda, Betic Cordilleras)
A1 Fernández Fernández, Estefanía
A1 Campos, J.
A1 González Lodeiro, Francisco
AB The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of movement. Later overturned north-vergent folds and brittle deformations associated to normal faults with a top-to-the-westsouthwest sense of movement affect the previous structures. The normal fault (Alcaucm Fault) that separates the Sierra Tejeda Unit (footwall) from the Canillas and Sayalonga Units (hanging wall) is a detachment. Normal faults that separate the different units of the hanging wall joint the detachment and they do not penetrate into the footwall
PB Sociedad Geológica de España
YR 1992
FD 1992
LK http://hdl.handle.net/10272/16337
UL http://hdl.handle.net/10272/16337
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026