Sismicidad en el antepaís de las cordilleras Béticas orientalesdeterminación del tensor de esfuerzos actual.

  1. Rincón, P. J. 1
  2. Giner, J. 1
  3. Vegas, R. 1
  4. De Vicente, G. 1
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1996

Zenbakien izenburua: Comunicaciones presentadas en el IV Congreso Nacional de Geología, Alcalá de Henares, 1996

Zenbakia: 20

Orrialdeak: 932-935

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

The seismicity in the Castilian foreland of the Betic Cordilleras is in accordance with an in traplate compressive stress-field that is characterized by the coexistence of two stress tensors: SHmax N7 40º-160ºE (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 sorne N130º-1 SOºE fault zones in the front of the Alcaraz Arc.

Datuen iturria: Dialnet