RT Conference Proceedings
T1 El despegue extensional de Lahsene y los jirones de serpentinitas del anticlinal de Taryat (Melilla, Rif)
T1 The Lahsene extensional detachment and the serpentinite slices of the Taryat anticline (Melilla, Rif)
A1 García Dueñas, V.
A1 Balanyá, Juan Carlos
A1 Sánchez Gómez, Mario
AB The Taryat anticline, between Melilla and the Cabo Tres Forcas, folds an extensional detachment fault with SW transport sense. The fault is sealed by Tortonian marine sediments that were also folded.The hanging wall of the detachment is made up of brecciated slates andred sandstones, and the footwall consists of phyllites with chloritoid. These rock formations can be respectively attributed to the Maiaguide and Alpujarride complexes. Several serpentinite slices form part of the fault breccia
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/13837
UL http://hdl.handle.net/10272/13837
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026