Historia geológica de la cuenca de Lorca (Murcia): influencia de la tectónica en la sedimentación

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dc.contributor.authorGuillén Mondéjar, F.
dc.contributor.authorRodríguez Estrella, Tomás
dc.contributor.authorArana, R.
dc.contributor.authorLópez Aguayo, F.
dc.date.accessioned2017-03-23T12:34:35Z
dc.date.available2017-03-23T12:34:35Z
dc.date.issued1995
dc.description.abstractNeogene sedimentation in the Lorca basin has been related to tectonics specially to Basin's Central Fault, whic has alternately like inverse and normal according to compressive ord is tensible phases; likewise the depocentre has been displaced successively to one side and the other of the fore-mentioned accident.en_US
dc.identifier.urihttp://hdl.handle.net/10272/13522
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.otherLorca basinen_US
dc.subject.otherNeogeneen_US
dc.subject.otherPaleogeographic evolutionen_US
dc.titleHistoria geológica de la cuenca de Lorca (Murcia): influencia de la tectónica en la sedimentaciónen_US
dc.titleGeologic history of the Lorca basin (Murcia): influence of tectonics on sedimentationeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)