Deslizamientos de bajo ángulo en la Cuenca de Baza (Cordillera Bética)

  1. L. Gilbert
  2. C. Sanz de Galdeano
  3. P. Alfaro
  4. A.C. López Garrido
  5. G. Scott
Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2003

Zenbakien izenburua: V Congreso del Grupo Español del Terciario (Granada, 23-25 de septiembre, 2003)

Zenbakia: 5

Orrialdeak: 95-97

Mota: Artikulua

DIALNET GOOGLE SCHOLAR lock_openSarbide irekia editor

Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

The NE sector of the Baza basin shows Pleistocene very peculiar low angle landslides, that advance towards the N-NE in a deltaic environment. The landslides occurred in a period of regional tectonic activity implying important changes in the source areas of the detrital deposits. The most probably cause which trigger the movement was an earthquake.

Datuen iturria: Dialnet