RT Conference Proceedings
T1 La falla normal de bajo ángulo de Tejeda: un ejemplo de la deformación miocena en las Béticas centrales
T1 The Tejeda low-angle normal fault: an example of mlocene deformation in the Central Betics
A1 Alonso Chaves, Francisco Manuel
A1 Orozco, Miguel
A1 García Dueñas, V.
A1 Mayoral Alfaro, Eduardo
AB The existence of a major extensional fault in Sierra Tejeda, Central Betics, developed during the middle Miocene, is evidenced. The Tejeda, Venta de Palma, Bentomiz and Alcaiceria units make up the hanging-wall o f the fault. These units are tilted tow ard the N and NE. The collapse of the thinned crust of Alboran Domain is related with extensional origin of the contacts between units. Middle MioceneTortonian age deposits of the Granada basin seal the Tejeda extensional fault (FET)
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/13882
UL http://hdl.handle.net/10272/13882
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026