RT Journal Article
T1 ¿Por qué son tan diferentes las sierras de Crevillente y Abanilla?
T1 Why are so different the Crevillente and Abanilla mountain ranges ?
A1 Tent Manclús, José Enrique
A1 Yébenes, Alfonso
A1 Estévez, Antonio
AB The Crevillente and Abanilla mountain ranges form the same structural lineation but show a quite differentmorphology. The first one is made by calcareous rocks mainly jurassic and cretaceous likewise the Abanillais made by keuper facies which includes blocks. This keuper facies are not Triassic but Miocene which areinterpreted as an ancient salt glacier. Their different litologies of both sierras is due to the activity of thePuerto de Barinas Fault, a transverse fault to the Crevillente-Abanilla lineament. This litological differencein the same structural lineament could be explained as produced before (pre-late Tortonian) the elevationof both sierras (latest Messinian)
PB Sociedad Geológica de España
YR 2004
FD 2004
LK http://hdl.handle.net/10272/8889
UL http://hdl.handle.net/10272/8889
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026