Téctonica y sedimentación en el margen oeste del «rift» terciario del valle de Ayora-Cofrentes (Valencia).

  1. Santisteban Bové, Carlos de
  2. Saiz, J.
  3. Bello, D.
  4. Ruiz Sánchez, Francisco Javier
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1990

Zenbakia: 8

Orrialdeak: 44-47

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

The Ayora-Cofrentes valley (Valencia) presents a rift-like structure of probable Lower Tertiary age. Its western margin is formed by a system of lystric faults with a vertical displacement of 300 m. This main fault is affected by a zone of dextral E-W strike-slip, which caused the development of a symmetrical graben. This structure is active since the Tertiary.

Datuen iturria: Dialnet