@article{10272/12669,
year = {1996},
url = {http://hdl.handle.net/10272/12669},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Sismicidad en el antepaís de las cordilleras Béticas orientales: determinación del tensor de esfuerzos actual},
title = {Seismicity in the castillan forelandl of de betic cordilleras: neotectonic stress tensor determination},
author = {Rincón Calero, P. J. and Giner Robles, J. L. and Vegas, Ramón and Vicente, Gerardo de},
}