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Article: Sedimentary provenance of the Hengyang and Mayang basins, SE China, and implications for the Mesozoic topographic change in South China Craton: Evidence from detrital zircon geochronology

TitleSedimentary provenance of the Hengyang and Mayang basins, SE China, and implications for the Mesozoic topographic change in South China Craton: Evidence from detrital zircon geochronology
Authors
KeywordsHengyang Basin
Provenance
South China Craton
Topography Transition
Zircon Geochronology
Issue Date2011
PublisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/jseaes
Citation
Journal Of Asian Earth Sciences, 2011, v. 41 n. 6, p. 494-503 How to Cite?
AbstractDetrital zircon U-Pb data from sedimentary rocks in the Hengyang and Mayang basins, SE China reveal a change in basin provenance during or after Early Cretaceous. The results imply a provenance of the sediment from the North China Craton and Dabie Orogen for the Upper Triassic to Middle Jurassic sandstones and from the Indosinian granitic plutons in the South China Craton for the Lower Cretaceous sandstones. The 90-120. Ma age group in the Upper Cretaceous sandstones in the Hengyang Basin is correlated with Cretaceous volcanism along the southeastern margin of South China, suggesting a coastal mountain belt have existed during the Late Cretaceous. The sediment provenance of the basins and topographic evolution revealed by the geochronological data in this study are consistent with a Mesozoic tectonic setting from Early Mesozoic intra-continental compression through late Mesozoic Pacific Plate subduction in SE China. © 2011 Elsevier Ltd.
Persistent Identifierhttp://hdl.handle.net/10722/151312
ISSN
2015 Impact Factor: 2.647
2015 SCImago Journal Rankings: 1.393
ISI Accession Number ID
Funding AgencyGrant Number
Chinese Academy of SciencesKZCX1-YW-15-1
National Natural Science Foundation of China40773004
40776024
Funding Information:

We thank Dr Andrew Carter from London Thermochronology Research Group, University College London for helpful comments. This work was financially co-supported by the Chinese Academy of Sciences (No. KZCX1-YW-15-1), the National Natural Science Foundation of China (Nos. 40773004 and 40776024). This is Contribution No. IS-1326 from GIGCAS.

References

 

DC FieldValueLanguage
dc.contributor.authorYan, Yen_US
dc.contributor.authorHu, XQen_US
dc.contributor.authorLin, Gen_US
dc.contributor.authorSantosh, Men_US
dc.contributor.authorChan, LSen_US
dc.date.accessioned2012-06-26T06:20:27Z-
dc.date.available2012-06-26T06:20:27Z-
dc.date.issued2011en_US
dc.identifier.citationJournal Of Asian Earth Sciences, 2011, v. 41 n. 6, p. 494-503en_US
dc.identifier.issn1367-9120en_US
dc.identifier.urihttp://hdl.handle.net/10722/151312-
dc.description.abstractDetrital zircon U-Pb data from sedimentary rocks in the Hengyang and Mayang basins, SE China reveal a change in basin provenance during or after Early Cretaceous. The results imply a provenance of the sediment from the North China Craton and Dabie Orogen for the Upper Triassic to Middle Jurassic sandstones and from the Indosinian granitic plutons in the South China Craton for the Lower Cretaceous sandstones. The 90-120. Ma age group in the Upper Cretaceous sandstones in the Hengyang Basin is correlated with Cretaceous volcanism along the southeastern margin of South China, suggesting a coastal mountain belt have existed during the Late Cretaceous. The sediment provenance of the basins and topographic evolution revealed by the geochronological data in this study are consistent with a Mesozoic tectonic setting from Early Mesozoic intra-continental compression through late Mesozoic Pacific Plate subduction in SE China. © 2011 Elsevier Ltd.en_US
dc.languageengen_US
dc.publisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/jseaesen_US
dc.relation.ispartofJournal of Asian Earth Sciencesen_US
dc.subjectHengyang Basinen_US
dc.subjectProvenanceen_US
dc.subjectSouth China Cratonen_US
dc.subjectTopography Transitionen_US
dc.subjectZircon Geochronologyen_US
dc.titleSedimentary provenance of the Hengyang and Mayang basins, SE China, and implications for the Mesozoic topographic change in South China Craton: Evidence from detrital zircon geochronologyen_US
dc.typeArticleen_US
dc.identifier.emailChan, LS:chanls@hku.hken_US
dc.identifier.authorityChan, LS=rp00665en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.1016/j.jseaes.2011.03.012en_US
dc.identifier.scopuseid_2-s2.0-79955580837en_US
dc.identifier.hkuros214223-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-79955580837&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume41en_US
dc.identifier.issue6en_US
dc.identifier.spage494en_US
dc.identifier.epage503en_US
dc.identifier.isiWOS:000291773000002-
dc.publisher.placeUnited Kingdomen_US
dc.identifier.scopusauthoridYan, Y=36490767800en_US
dc.identifier.scopusauthoridHu, XQ=49963592000en_US
dc.identifier.scopusauthoridLin, G=7401699881en_US
dc.identifier.scopusauthoridSantosh, M=7005398812en_US
dc.identifier.scopusauthoridChan, LS=7403540528en_US
dc.identifier.citeulike9192834-

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