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Sedimentary environment and stratigraphic ciclicity of the Lower Cretaceous «Arenas y arcillas del Collado» Formation, in Alpuente (Valencia)

dc.contributor.authorSantisteban, Carlos de
dc.date.accessioned2014-10-24T08:33:31Z
dc.date.available2014-10-24T08:33:31Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10272/8967
dc.description.abstractThe «Arenas y arcillas del Collado» Formation (Lower Cretaceous, Southwestern Iberian Basin, Valencia) represent a wave-dominated delta. It contain fluvial and shallow- marine deposits wich are arranged in two types of high-frequency sequences. The first type (up to 2 m thick) is a transgressive - regressive parasequence formed by shoreface to fluvial deposits. The second type (up to 15 m thick) is a composite depositional sequence formed by four to six parasequences. The lower part of each deoositional sequence contain a progradational thick group of shoreface / foreshore sandstone units, which sharply overlies an erosional surface modified by waves during transgressionen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherWave-dominated deltaen_US
dc.subject.otherFive order ciclicityen_US
dc.subject.otherLower Cetaceousen_US
dc.subject.otherSouthwestern Iberian Basinen_US
dc.subject.otherValenciaen_US
dc.titleAmbiente sedimentario y ciclicidad estratigrafica de los materiales de la Formacion «Arenas y ardllas del Collado» (Cretacico inferior), en el sector de Alpuente (Valencia)en_US
dc.titleSedimentary environment and stratigraphic ciclicity of the Lower Cretaceous «Arenas y arcillas del Collado» Formation, in Alpuente (Valencia)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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