RT Journal Article
T1 Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
T1 Neotectonics in the Castilian foreland of the Betic cordilleras
A1 Rincón Calero, P. J.
A1 Vegas, Ramón
AB The major morphotectonic features in the foreland of the Eastern Betics can be explained within the frame of the weak compressive stress field originated in the Prebetic fold and thrust belt. This NW directed compression is partitioned by N130°-150° dextral strike-slip corridors and orthogonal crustal flexures. The Neogene-Quaternary volcanism and the distribution of seismicity can be also considered within this compressive neotectonic regimen
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12661
UL http://hdl.handle.net/10272/12661
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026