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

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Texte intégral

lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

D'autres publications dans: Geogaceta

Résumé

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.

La source de données: Dialnet