@article{10272/9529,
year = {2001},
url = {http://hdl.handle.net/10272/9529},
abstract = {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},
publisher = {Sociedad Geológica de España},
keywords = {Neotectonics},
keywords = {Active tectonics},
keywords = {Betic Cordillera},
keywords = {Granada Basin},
title = {Estructura y tectónica activa del Valle de Lecrín (Granada)},
title = {Structure and active tectonics in the Lecrín Valley (Granada)},
author = {Sanz de Galdeano, Carlos and López Garrido, Ángel Carlos},
}