RT Journal Article
T1 Características geológicas de la Sierra de Quibas (Abanilla, Murcia). Su relación con un yacimiento paleontológico pleistoceno
T1 Geological characteristics of the Sierra de Quibas (Abanilla, Murcia). Relationship with a Pleistocenepaleontological site
A1 Rodríguez Estrella, Tomás
A1 Mancheño, Miguel Ángel
A1 Romero, G.
A1 Hernández, J. M.
AB The Sierra de Quibas is mainly a Lower Jurassic carbonated relief. Its main structure is a klippe of Middle Subbeticon Southern Prebetic. The internal structure is a NE-SW anticlinorium. Detailed geological mapping (E. 1:25,000) has pointed to anomalous folds (almost N-S) caused by the halokinétic action ofTriassic materials. Also has been detected a Neotectonic activity starting in the Upper Miocene with almost N-S stresses which have reactivated some faults; the N-S faults previously compressive are now distensive.In the SE edge of the Sierra de Quibas there is an important Pleistocene paleontological site in a karstic cave filled up with reddish detritic material within the Lower Jurassic dolomites, controlled by NE-SW faults
PB Sociedad Geológica de España
YR 2003
FD 2003
LK http://hdl.handle.net/10272/8972
UL http://hdl.handle.net/10272/8972
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026