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Sedimentary Architecture and Sequence Stratigraphy of Upper Cenomanian-Uppermost Cenomanian. Central Iberian Range

dc.contributor.authorMartínez, P.
dc.contributor.authorMeléndez Hevia, Alfonso
dc.date.accessioned2015-05-08T08:49:45Z
dc.date.available2015-05-08T08:49:45Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10520
dc.description.abstractThe D.S. «Cabrejas del Pinar» is recorded during upper Cenomanian-uppermost Cenomanian. The low system tract is not recorded. No clear evidences for the high system tracts and similar facies on the field between two overlaping transgressive system tracts make difficult to identify and correlate the boundary along the ramp. The D.S is represented in the area by mid ramp facies consisting of nodular limestones developing SE to shallower nodular deposits with sedimentary structures. The thickness is ranging from 12 m at the NW to 4 m at the southeasternmost part. The T.5.T. is composed by four parasequences with onlap geometry and retrogradational evolution southeastward. The parasequences space distribution Is conditioned by the paleogeography and configuration of the ramp of NO poralltyen_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.otherCarbonate rampen_US
dc.subject.otherDepositional sequencesen_US
dc.subject.otherUppermost Cenomanianen_US
dc.subject.otherParasequencesen_US
dc.titleArquitectura sedimentaria y estratigrafía secuencial del Cenomaniense superior-Cenomaniense terminal. Cordillera Ibérica Centralen_US
dc.titleSedimentary Architecture and Sequence Stratigraphy of Upper Cenomanian-Uppermost Cenomanian. Central Iberian Rangeeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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