Características geológicas de la Sierra de Quibas (Abanilla, Murcia). Su relación con un yacimiento paleontológico pleistoceno

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dc.contributor.authorRodríguez Estrella, Tomás
dc.contributor.authorMancheño, Miguel Ángel
dc.contributor.authorRomero, G.
dc.contributor.authorHernández, J. M.
dc.date.accessioned2014-10-24T09:44:52Z
dc.date.available2014-10-24T09:44:52Z
dc.date.issued2003
dc.description.abstractThe 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 faultsen_US
dc.identifier.urihttp://hdl.handle.net/10272/8972
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSierra de Quibctsen_US
dc.subject.otherStratigraphyen_US
dc.subject.otherTectonicen_US
dc.subject.otherNeotectonicen_US
dc.subject.otherPleistocene paleontological siteen_US
dc.titleCaracterísticas geológicas de la Sierra de Quibas (Abanilla, Murcia). Su relación con un yacimiento paleontológico pleistocenoen_US
dc.titleGeological characteristics of the Sierra de Quibas (Abanilla, Murcia). Relationship with a Pleistocene paleontological siteeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 35, (2003)