RT Journal Article
T1 Nuevos datos sobre comprensión pleistocena en el extremo oriental del Algarve (Portugal)
T1 New data about Pleistocene compression in the eastern edge of Algarve (Portugal)
A1 Flores Hurtado, Enrique
A1 Rodríguez Vidal, Joaquín
A1 Cáceres Puro, Luis Miguel
AB The end of the Pliocene was characterized by a return to the compressive regime throughout the southern of the Iberian peninsula. Quaternary deformations are intense in places and correspond to folds and occasionally reversal faults.At the western sector of the Guadalquivir basin the neotectonic activity is not still investigated. The studied section shows folded Quaternary terrace deposits and sometimes crushed terraces between mesozolc rock bodies. The entire studied outcrop looks as a WSW-ENEAW-E fault zone that, also a possible previous activity, it would support strain, at least compressive, contemporary to the terrace deposits (Pleistocene).
PB Sociedad Geológica de España
YR 1993
FD 1993
LK http://hdl.handle.net/10272/14053
UL http://hdl.handle.net/10272/14053
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026