RT Journal Article
T1 Turbiditas calcáreas y otros fenómenos de resedimentación/ erosión en el Jurásico superior-Cretácico inferior de la unidad de Huelma (Jaén). Zonas Externas de las cordilleras Béticas
T1 Carbonate turbidites and other resedimentation/erosion processes in the Upper Jurassic-Lower Cretaceous of the Huelma unit (Jaén). External Zones of the Betic cordillera
A1 Ruiz Ortiz, Pedro Alejandro
A1 Molina, José Miguel
A1 Nieto, Luis M.
AB Carbonate turbidites made up by conglomerates and calcarenites are interpreted as a base-of-slope apron. The slope was, probably, the transition between the trough of the Intermediate domain and the External Subbetic swell. This slope was a place of erosion and resedimentation during the Late Jurassic and Early Cretaceous, in relation with two main tectonic events which resulted in the erosion of the platform margin and turbidite deposition
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12217
UL http://hdl.handle.net/10272/12217
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026