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

Carlos de Santisteban Bové, J. Saiz, D. Bello, Francisco Javier Ruiz Sánchez

• 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.