@article{10272/8972,
year = {2003},
url = {http://hdl.handle.net/10272/8972},
abstract = {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},
publisher = {Sociedad Geológica de España},
keywords = {Sierra de Quibcts},
keywords = {Stratigraphy},
keywords = {Tectonic},
keywords = {Neotectonic},
keywords = {Pleistocene paleontological site},
title = {Características geológicas de la Sierra de Quibas (Abanilla, Murcia). Su relación con un yacimiento paleontológico pleistoceno},
title = {Geological characteristics of the Sierra de Quibas (Abanilla, Murcia). Relationship with a Pleistocene

paleontological site},
author = {Rodríguez Estrella, Tomás and Mancheño, Miguel Ángel and Romero, G. and Hernández, J. M.},
}