Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/654
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dc.contributor.authorMoseley, Gina E.-
dc.contributor.authorRichards, David A.-
dc.contributor.authorSmith, Christopher J. M.-
dc.contributor.authorSmart, Peter L.-
dc.contributor.authorHoffmann, Dirk-
dc.contributor.authorFarrant, Andrew R. ‎-
dc.date.accessioned2018-08-20T14:22:05Z-
dc.date.issued2013-04-
dc.identifier.citationCave and Karst Science, 2013, 40 (1), 13-16es_ES
dc.identifier.issn1356-191X-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/654-
dc.description.abstractThe Gunung Mulu National Park, Sarawak, Malaysia has been a focus of scientific research and exploration for several decades. Previous work investigated the relationship between fluvial incision into the limestone massif and the chronological evolution of the 500m-deep network of cave passages. This study involved analyses of newly available speleothem material using state-of-the-art U–Th dating methods and assessment of the potential for extension of the chronological record using U–Pb dating techniques.es_ES
dc.language.isoenes_ES
dc.publisherBritish Cave Research Associationes_ES
dc.rightsinfo:eu-repo/semantics/closedAccess-
dc.titleU–Th dating of speleothems to investigate the evolution of limestone caves in the Gunung Mulu National Park, Sarawak, Malaysiaes_ES
dc.typeArticlees_ES
dc.relation.publisherversionhttp://bcra.org.uk/pub/candks/index.html?j=118es_ES
dc.date.available2018-08-20T14:22:05Z-
Appears in Collections:Geocronología y Geología



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