Secuencias deposicionales del Cretácico en el flanco sur del Sistema Central

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dc.contributor.authorGil, J.
dc.contributor.authorGarcía, A.
dc.contributor.authorSegura, M.
dc.date.accessioned2017-11-10T11:01:23Z
dc.date.available2017-11-10T11:01:23Z
dc.date.issued1992
dc.description.abstractEight depositional sequences have been recognized in the Cretaceous of the southern border of the Central System. The thickness of sedimentary succession, the marine character of the sediments and the number of depositional sequences decrease westwards. It is possible to recognize a stratigraphic structure in onlap with diacronic distribution of the dolostones, marls and terrigenous facies. This stratigraphic succession is related to the Cretaceous of the Nothern Iberian Ranges and from a paleogeographical point of view, i t correlates to the Atlantic Margin of the Iberian Plate. Its age is Cenomanian to Campanian.es_ES
dc.identifier.urihttp://hdl.handle.net/10272/14146
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherDepositional sequenceses_ES
dc.subject.otherCretaceouses_ES
dc.subject.otherCentral Mountainses_ES
dc.subject.otherSpaines_ES
dc.titleSecuencias deposicionales del Cretácico en el flanco sur del Sistema Centrales_ES
dc.titleCretaceous depositional sequences in the southern margin of the Central System, Spaineng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 13, (1992)