El pliegue sinsedimentario de Hinojares (sector de Pozo Alcón-Tíscar, provincia de Jaén, zona externa bética)

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dc.contributor.authorSanz de Galdeano, Carlos
dc.contributor.authorGalindo Zaldívar, Jesús
dc.contributor.authorLópez Garrido, Ángel Carlos
dc.contributor.authorAlfaro García, Pedro
dc.contributor.authorRuiz Bustos, A.
dc.contributor.authorMarín Lechado, Carlos
dc.date.accessioned2014-07-09T08:36:15Z
dc.date.available2014-07-09T08:36:15Z
dc.date.issued2006
dc.description.abstractIn the proximities of Hinojares (northern border of the Guadix-Baza basin), there is a growth syncline, formed in Plio-Quaternary sediments, showing progressive unconformities in its limbs. At its ESE prolongation, the recent glacis, Pleistocene in age, shows two flexions parallel to the fold hinge and limbs. This fold has been probably controlled by the Tiscar fault and formed within a NNE-SSW compressive settingen_US
dc.identifier.urihttp://hdl.handle.net/10272/8466
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherGrowth synclineen_US
dc.subject.otherNeotectonicsen_US
dc.subject.otherActive Tectonicsen_US
dc.subject.otherGuadix-Baza basinen_US
dc.subject.otherRodent toothen_US
dc.titleEl pliegue sinsedimentario de Hinojares (sector de Pozo Alcón-Tíscar, provincia de Jaén, zona externa bética)en_US
dc.titleThe Hinojares synsedimentary fold (Pozo Alcón-Tíscar area, Jaen province, Betic External Zone)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 41, (2006)