RT Journal Article
T1 Estructura y tectónica activa del Valle de Lecrín (Granada)
T1 Structure and active tectonics in the Lecrín Valley (Granada)
A1 Sanz de Galdeano, Carlos
A1 López Garrido, Ángel Carlos
AB The structure of the Lecrin Valley is a graben, or a semigraben, formed by parallel E-W normal faults, mainly located in its southern part, where is limited by the Sierra de los Guajares. The throw of these faults is of the order of 1200 m in its eastern part, but progressively diminishing westwards. These faults moved especially between the Late Miocene and the Pliocene?-Quaternary, but their most recent displacements affect even the Quaternary glads. This valley is the scenary of a very important fluvial incision, within a very active process of regional uplift
PB Sociedad Geológica de España
YR 2001
FD 2001
LK http://hdl.handle.net/10272/9529
UL http://hdl.handle.net/10272/9529
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 15 jul 2026