File Download
  Links for fulltext
     (May Require Subscription)
  • Find via Find It@HKUL
Supplementary

Article: Grain-size cycles in Salawusu River valley since 150 ka BP

TitleGrain-size cycles in Salawusu River valley since 150 ka BP
Authors
KeywordsSalawusu River valley
Milanggouwan section
150 ka BP
Grain-size
Palaeoclimate cycles
Issue Date2001
PublisherScience Press. The Journal's web site is located at http://www.maney.co.uk/geographical.html
Citation
Journal of Geographical Sciences, 2001, v. 11 n. 4, p. 461-472 How to Cite?
AbstractThe palaeo-mobile dune sands and fluvio-lacustrine facies with palaeosols in Milanggouwan stratigraphic section of the Salawusu River valley situated at the southeast of the Mu Us Desert experienced abundant remarkable alternative changes of coarse and fine rhythms in grainsize since 150 ka BP, and the grain-size parameters — Mz, σ, Sk, Kg and SC/D also respond to the situation of multi-fluctuational alternations between peak and valley values. Simultaneity the grainsize eigenvalues — ϕ5, ϕ16, ϕ25, ϕ50, ϕ75, ϕ84 and ϕ95 are respondingly manifested as greatly cadent jumpiness. Hereby, the Milanggouwan section can be divided into 27 grain-size coarse and fine sedimentary cycles, which can be regarded as a real and integrated record of climate-geological process of desert vicissitude resulted from the alternative evolvement of the ancient winter and summer monsoons of East Asia since 150 ka BP.
Persistent Identifierhttp://hdl.handle.net/10722/86071
ISSN
2014 Impact Factor: 1.344
2014 SCImago Journal Rankings: 0.573

 

DC FieldValueLanguage
dc.contributor.authorZhang, Yen_HK
dc.contributor.authorLi, Ben_HK
dc.contributor.authorJin, Hen_HK
dc.contributor.authorZhang, DDen_HK
dc.contributor.authorYan, Men_HK
dc.contributor.authorZhu, Yen_HK
dc.contributor.authorYao, Cen_HK
dc.date.accessioned2010-09-06T09:12:32Z-
dc.date.available2010-09-06T09:12:32Z-
dc.date.issued2001en_HK
dc.identifier.citationJournal of Geographical Sciences, 2001, v. 11 n. 4, p. 461-472en_HK
dc.identifier.issn1009-637Xen_HK
dc.identifier.urihttp://hdl.handle.net/10722/86071-
dc.description.abstractThe palaeo-mobile dune sands and fluvio-lacustrine facies with palaeosols in Milanggouwan stratigraphic section of the Salawusu River valley situated at the southeast of the Mu Us Desert experienced abundant remarkable alternative changes of coarse and fine rhythms in grainsize since 150 ka BP, and the grain-size parameters — Mz, σ, Sk, Kg and SC/D also respond to the situation of multi-fluctuational alternations between peak and valley values. Simultaneity the grainsize eigenvalues — ϕ5, ϕ16, ϕ25, ϕ50, ϕ75, ϕ84 and ϕ95 are respondingly manifested as greatly cadent jumpiness. Hereby, the Milanggouwan section can be divided into 27 grain-size coarse and fine sedimentary cycles, which can be regarded as a real and integrated record of climate-geological process of desert vicissitude resulted from the alternative evolvement of the ancient winter and summer monsoons of East Asia since 150 ka BP.-
dc.languageengen_HK
dc.publisherScience Press. The Journal's web site is located at http://www.maney.co.uk/geographical.htmlen_HK
dc.relation.ispartofJournal of Geographical Sciencesen_HK
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License-
dc.subjectSalawusu River valley-
dc.subjectMilanggouwan section-
dc.subject150 ka BP-
dc.subjectGrain-size-
dc.subjectPalaeoclimate cycles-
dc.titleGrain-size cycles in Salawusu River valley since 150 ka BPen_HK
dc.typeArticleen_HK
dc.identifier.emailZhang, DD: zhangd@hkucc.hku.hken_HK
dc.identifier.authorityZhang, DD=rp00649en_HK
dc.description.naturepublished_or_final_version-
dc.identifier.hkuros71498en_HK
dc.identifier.volume11-
dc.identifier.issue4-
dc.identifier.spage461-
dc.identifier.epage472-
dc.publisher.placeChina-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats