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DOI10.1016/j.geomorph.2009.06.016
OSL dating of glacier extent during the Last Glacial and the Kanas Lake basin formation in Kanas River valley, Altai Mountains, China
Xu, Xiangke; Yang, Jianqiang; Dong, Guocheng; Wang, Liqiang; Miller, Lee
通讯作者Yang, JQ (通讯作者)
发表日期2009
ISSN0169-555X
EISSN1872-695X
起始页码306
结束页码317
卷号112期号:3-4
英文摘要The Kanas River originates on the southern slope of Youyi Peak, the largest center of modern glaciers in Altai Mountains, China. Three sets of moraines and associated glacial sediments are well preserved near the Kanas Lake outlet, recording a complex history and landscape evolution during the Last Glacial. Dating the moraines allows the temporal and spatial glacier shift and climate during the Last Glacial to be determined, and then constrains when and how the Kanas Lake basin was formed. Dating of the glacial tills was undertaken by utilizing the optically stimulated luminescence (OSL) method. Results date four samples from the three sets of moraines to 28.0, 34.4,38.1, and 49.9 ka and one sample from outwash sediment to 6.8 ka. The Kanas Lake basin is a clownfaulted basin and was eroded by glacier before 28.0 ka, and the glacial moraines blocked the glacier-melt water after the glacier retreat, which made the present-day Kanas Lake eventually form at least before 6.8 ka BP. In Altai Mountains, the glacier advance was more extensive in Marine Isotope Stage (MIS) 3 than MIS 2, probably because the mid-latitude westerlies shifted northward and/or intensified during the MIS 3, resulting in a more positive glacier mass balance. Nevertheless, the Siberian High dominated the Altai Mountains in MIS 2, resulting in a relative decrease in precipitation. (C) 2009 Elsevier B.V. All rights reserved.
关键词LATE QUATERNARY GLACIATIONEASTERN HINDU-KUSHNORTHERN PAKISTANURUMQI RIVERHUNZA VALLEYLUMINESCENCESEDIMENTSPLEISTOCENECHRONOLOGYHIMALAYA
英文关键词Kanas River valley; Glacial erosion; Numerical dating; Last Glacial; Paleoclimate
语种英语
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000270640600010
来源期刊GEOMORPHOLOGY
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/257651
推荐引用方式
GB/T 7714
Xu, Xiangke,Yang, Jianqiang,Dong, Guocheng,et al. OSL dating of glacier extent during the Last Glacial and the Kanas Lake basin formation in Kanas River valley, Altai Mountains, China[J]. 中国科学院青藏高原研究所,2009,112(3-4).
APA Xu, Xiangke,Yang, Jianqiang,Dong, Guocheng,Wang, Liqiang,&Miller, Lee.(2009).OSL dating of glacier extent during the Last Glacial and the Kanas Lake basin formation in Kanas River valley, Altai Mountains, China.GEOMORPHOLOGY,112(3-4).
MLA Xu, Xiangke,et al."OSL dating of glacier extent during the Last Glacial and the Kanas Lake basin formation in Kanas River valley, Altai Mountains, China".GEOMORPHOLOGY 112.3-4(2009).
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