Deslizamientos de bajo ángulo en la Cuenca de Baza (Cordillera Bética)
- L. Gilbert
- C. Sanz de Galdeano
- P. Alfaro
- A.C. López Garrido
- G. Scott
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
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.