File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Late pleistocene evolution of Lake Manas in western China with constraints of OSL ages of lacustrine sediments

TitleLate pleistocene evolution of Lake Manas in western China with constraints of OSL ages of lacustrine sediments
Authors
KeywordsChronology
Climate variation
Eolian deposit
Holocene
Lacustrine deposit
Issue Date2012
PublisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/wps/find/journaldescription.cws_home/706731/description?navopenmenu=1
Citation
Quaternary Geochronology, 2012, v. 10, p. 143-149 How to Cite?
AbstractLake Manas, located in northwestern China, has been formed in a structure depression since early Quaternary. Optically stimulated luminescence (OSL) dating is applied to the lacustrine and aeolian deposits collected from the lake to construct a chronological frame for lake level fluctuations since the last inter-glacial period. The results yielded two stages of high lake stands (∼20 m above the present lake bed) occurred before 66 ka and 38-27 ka ago. No evidence for Holocene high lake level was found in the studying area. © 2012 Elsevier B.V.
Persistent Identifierhttp://hdl.handle.net/10722/163959
ISSN
2015 Impact Factor: 3.142
2015 SCImago Journal Rankings: 1.931
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorFan, Aen_US
dc.contributor.authorLi, SHen_US
dc.contributor.authorChen, YGen_US
dc.date.accessioned2012-09-20T07:53:57Z-
dc.date.available2012-09-20T07:53:57Z-
dc.date.issued2012en_US
dc.identifier.citationQuaternary Geochronology, 2012, v. 10, p. 143-149en_US
dc.identifier.issn1871-1014-
dc.identifier.urihttp://hdl.handle.net/10722/163959-
dc.description.abstractLake Manas, located in northwestern China, has been formed in a structure depression since early Quaternary. Optically stimulated luminescence (OSL) dating is applied to the lacustrine and aeolian deposits collected from the lake to construct a chronological frame for lake level fluctuations since the last inter-glacial period. The results yielded two stages of high lake stands (∼20 m above the present lake bed) occurred before 66 ka and 38-27 ka ago. No evidence for Holocene high lake level was found in the studying area. © 2012 Elsevier B.V.-
dc.languageengen_US
dc.publisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/wps/find/journaldescription.cws_home/706731/description?navopenmenu=1-
dc.relation.ispartofQuaternary Geochronologyen_US
dc.subjectChronology-
dc.subjectClimate variation-
dc.subjectEolian deposit-
dc.subjectHolocene-
dc.subjectLacustrine deposit-
dc.titleLate pleistocene evolution of Lake Manas in western China with constraints of OSL ages of lacustrine sedimentsen_US
dc.typeArticleen_US
dc.identifier.emailLi, SH: shli@hku.hken_US
dc.identifier.authorityLi, SH=rp00740en_US
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1016/j.quageo.2012.01.007-
dc.identifier.scopuseid_2-s2.0-84863781213-
dc.identifier.hkuros207872en_US
dc.identifier.volume10en_US
dc.identifier.spage143en_US
dc.identifier.epage149en_US
dc.identifier.isiWOS:000307195300023-
dc.publisher.placeNetherlands-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats