dc.contributorAcevedo, Rogelio Daniel
dc.creatorAcevedo, Rogelio Daniel
dc.date.accessioned2020-11-30T14:57:45Z
dc.date.accessioned2022-10-15T00:48:10Z
dc.date.available2020-11-30T14:57:45Z
dc.date.available2022-10-15T00:48:10Z
dc.date.created2020-11-30T14:57:45Z
dc.date.issued2019
dc.identifierAcevedo, Rogelio Daniel; The Cretaceous Layers Later than the Early Cretaceous; Springer; 2019; 33-36
dc.identifier978-3-030-00166-7
dc.identifierhttp://hdl.handle.net/11336/119351
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4326528
dc.description.abstractThe marine continuity after the Early Cretaceous implies an essential difference with the condition in the orogenic belt with a N-S trend of the Patagonian Cordillera. But this important difference does not avoid the matter concerning if these Late Cretaceous layers have been in fact involved in the same folding complexity as the Early Cretaceous ones, with slight metamorphism. The available information results, at present, not complete enough to adjust a formational definition.
dc.languageeng
dc.publisherSpringer
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007%2F978-3-030-00166-7_5
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1007/978-3-030-00166-7_5
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.sourceGeological Records of the Fuegian Andes Deformed Complex Outlined in a Patagonian Orogenic Belt Regional Context
dc.subjectUpper Cretaceous
dc.subjectInoceramus sp.
dc.subjectTierra del Fuego
dc.titleThe Cretaceous Layers Later than the Early Cretaceous
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeinfo:eu-repo/semantics/bookPart
dc.typeinfo:ar-repo/semantics/parte de libro


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