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- Publisher Website: 10.1016/j.quageo.2012.01.007
- Scopus: eid_2-s2.0-84863781213
- WOS: WOS:000307195300023
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Article: Late pleistocene evolution of Lake Manas in western China with constraints of OSL ages of lacustrine sediments
| Title | Late pleistocene evolution of Lake Manas in western China with constraints of OSL ages of lacustrine sediments |
|---|---|
| Authors | |
| Keywords | Chronology Climate variation Eolian deposit Holocene Lacustrine deposit |
| Issue Date | 2012 |
| Publisher | Elsevier 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? |
| Abstract | Lake 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 Identifier | http://hdl.handle.net/10722/163959 |
| ISSN | 2023 Impact Factor: 1.7 2023 SCImago Journal Rankings: 0.811 |
| ISI Accession Number ID |
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Fan, A | en_US |
| dc.contributor.author | Li, SH | en_US |
| dc.contributor.author | Chen, YG | en_US |
| dc.date.accessioned | 2012-09-20T07:53:57Z | - |
| dc.date.available | 2012-09-20T07:53:57Z | - |
| dc.date.issued | 2012 | en_US |
| dc.identifier.citation | Quaternary Geochronology, 2012, v. 10, p. 143-149 | en_US |
| dc.identifier.issn | 1871-1014 | - |
| dc.identifier.uri | http://hdl.handle.net/10722/163959 | - |
| dc.description.abstract | Lake 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.language | eng | en_US |
| dc.publisher | Elsevier BV. The Journal's web site is located at http://www.elsevier.com/wps/find/journaldescription.cws_home/706731/description?navopenmenu=1 | - |
| dc.relation.ispartof | Quaternary Geochronology | en_US |
| dc.subject | Chronology | - |
| dc.subject | Climate variation | - |
| dc.subject | Eolian deposit | - |
| dc.subject | Holocene | - |
| dc.subject | Lacustrine deposit | - |
| dc.title | Late pleistocene evolution of Lake Manas in western China with constraints of OSL ages of lacustrine sediments | en_US |
| dc.type | Article | en_US |
| dc.identifier.email | Li, SH: shli@hku.hk | en_US |
| dc.identifier.authority | Li, SH=rp00740 | en_US |
| dc.description.nature | link_to_subscribed_fulltext | - |
| dc.identifier.doi | 10.1016/j.quageo.2012.01.007 | - |
| dc.identifier.scopus | eid_2-s2.0-84863781213 | - |
| dc.identifier.hkuros | 207872 | en_US |
| dc.identifier.volume | 10 | en_US |
| dc.identifier.spage | 143 | en_US |
| dc.identifier.epage | 149 | en_US |
| dc.identifier.isi | WOS:000307195300023 | - |
| dc.publisher.place | Netherlands | - |
| dc.identifier.issnl | 1871-1014 | - |