RT Journal Article
T1 Escarpe de falla del Cuaternario reciente en la falla del Camp (Cadenas Costeras Catalanas)
T1 A late Quaternary fault scarp in the El Camp fault (Catalan Costal Ranges)
A1 Masana, E.
A1 Guimerà, J.
AB The activity of the El Camp fault since ear/y Neogene has originated the El Camp graben. We have defined at least three diferent Quaternary generations of al/uvial fans associated with the norma/ motion of that fault. The youngest movement which has caused morpho/ogical expression of the El Camp fault zone is in the Mont-roig fault, along which there are triangular facets and a fau/t scarp which involves a 33.000-75.000 year old alluvial fan —dated by arqueological methods (Lumley, 7971)—. Therefore, the Mont-roig fault has been active after 33.000-75.000 years BP.
PB Sociedad Geológica de España
YR 1991
FD 1991
LK http://hdl.handle.net/10272/17983
UL http://hdl.handle.net/10272/17983
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026