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dc.contributor.authorJiménez de Cisneros, C.
dc.contributor.authorLinares, J.
dc.contributor.authorReyes, E.
dc.contributor.authorVera, J. A.
dc.date.accessioned2020-06-26T10:12:10Z
dc.date.available2020-06-26T10:12:10Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/10272/18397
dc.description.abstractThe isotopic composition of modern calcite fills (onyx marble) in fractures and related caves is studied. Carbon and oxygen stable isotopes in this material are similar to the vadose speleothems (stalactites and stalagmites) in modern caves and to calcareous concretions in modern soils. This study can contribute to the recognition of analogous deposits in paleokarstses_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCalcite fillses_ES
dc.subject.otherOnyx marblees_ES
dc.subject.otherStable isotopeses_ES
dc.subject.otherPliocenees_ES
dc.subject.otherBetic Cordilleraes_ES
dc.titleIsótopos estables de carbono y oxígeno de los rellenos de calcita (falsa ágata) y su interés paleoambientales_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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