RT Journal Article
T1 Deformaciones tectónicas desde el Tortoniense en el Campo de Dalias (Cordilleras Béticas)
T1 Tectonic deformations since Tortonian in the Campo Je Dalias (Belie Cordilleras)
A1 Marín Lechado, Carlos
A1 Galindo Zaldívar, Jesús
A1 Rodríguez Fernández, L. R.
AB The Campo de Dalias is an emerged zone located at the northern boundary of Alboran Sea. The Neogene-Quaternary sediments of the Campo de Daifas are deformed by E-W open folds that also uplift Sierra de Cádor. The field studies reveals the existence of several joint sets with trends comprised between N170°E and N120°E some of them active at present. The oldest fault recognised in the region is normal, has an E-W trend, south dipping and is covered by Tortonian calcarenites. Other set of synsedimentary faults with N145°E trend deform Tortonian calcarenites. The best represented faults in the region are the Plio-Quaternary trastensional faults with dextral and sinistral components. Its trends are comprised between N170°E and N120°E and are compatible with a stress field ofSW-NE extension. These faults are mainly reactivated from previous joints and are active at present determining the coastline in the Balanegra fault zone
PB Sociedad Geológica de España
YR 2002
FD 2002
LK http://hdl.handle.net/10272/9157
UL http://hdl.handle.net/10272/9157
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026