Unidades tectosedimentarías y rupturas en la Cuenca de Lorca (Murcia)

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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.accessioned2017-06-12T12:06:52Z
dc.date.available2017-06-12T12:06:52Z
dc.date.issued1994
dc.description.abstractThe complementary use of the mineralógical and tectosedimentary analysis has allowed to establish five tectosedimentary units (TSU) in the Lorca Basin dated from the upper Burdigalian to the Pliocene. They were originated in marine environments with entrance of cotinental contributions except for the TSU-5, that has a fluvial-lacustrine origin. The absence of two tectosedimentary units at the north of the basin supported the existence of a fracture in the middle of the basin that has conditioned their space-temporal evolutionen_US
dc.identifier.urihttp://hdl.handle.net/10272/13801
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.otherTectosedimentary units (TSU)en_US
dc.subject.otherSedimentary breaksen_US
dc.titleUnidades tectosedimentarías y rupturas en la Cuenca de Lorca (Murcia)en_US
dc.titleTectosedimentary units and sedimentary breaks of the Lorca Basin (Murcia, Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 17, (1994)