RT Journal Article
T1 Sismicidad en el antepaís de las cordilleras Béticas orientales: determinación del tensor de esfuerzos actual
T1 Seismicity in the castillan forelandl of de betic cordilleras: neotectonic stress tensor determination
A1 Rincón Calero, P. J.
A1 Giner Robles, J. L.
A1 Vegas, Ramón
A1 Vicente, Gerardo de
AB The seismicity in the Castilian foreland of the Betic Cordilleras is in accordance with an intraplate compressive stress-field that is characterized by the coexistence of two stress tensors: SHmax N140°-160°E (regional tensor) and SHmax N60°-70°E (secondary tensor). The subsequent intraplate deformation is accommodated by means of dextral strike-slip faults and crustal flexures. The seismic activity seems to be concentrated in some N130°-150°E fault zones in the front of the Alcaraz Arc
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12669
UL http://hdl.handle.net/10272/12669
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026