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Extensive glacial advances during the Last Glacial Maximum near the eastern Himalayan syntaxis
Hu, G (Hu, Gang)1; Yi, CL (Yi, Chaolu)1; Zhang, JF (Zhang, Jiafu)2; Dong, GC (Dong, Guocheng)3,4; Liu, JH (Liu, Jinhua)1; Xu, XK (Xu, Xiangke)1; Jiang, T (Jiang, Tao)5; Hu, G
Source PublicationQUATERNARY INTERNATIONAL
2017
Volume443Issue:0Pages:1-12
DOI10.1016/j.quaint.2016.08.005
AbstractClimatically, the eastern Himalaya are mainly controlled by the Indian Summer Monsoon (ISM) and important region for understanding the relationship between ISM and glacial change. This region is therefore useful for studies of the relation between glacial changes and ISM. Using a geomorpho-stratigraphic method combined with GIS, we investigated and mapped the outmost lateral-frontal moraine of the most extensive glaciations that occurred in the Basongcuo (BSC) catchment, near the eastern Himalayan syntaxis. Using optically stimulated luminescence (OSL) and Be-10 surface exposure dating technique, we dated five boulders and 23 sediment samples. The resultant OSL and Be-10 ages show that the region's glaciers were at their most extensive positions between similar to 16 and 31 ka. Glacial coverage was 507.5 km(2), 9.9 times greater than it is today (51.5 km(2)), with an equilibrium line altitude (ELA) depression of similar to 690 m. The rapidity with which the Last Glacial Maximum (LGM) glacial advance and retreat occurred suggests that temperature was the dominant control on glacial change. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.
Subject Area自然地理学
WOS IDWOS:000406753900001
Language英语
Indexed BySCI
KeywordSoutheastern Tibetan Plateau Late Quaternary Glaciations Equilibrium-line Altitudes Regenerative-dose Protocol Late Pleistocene Cosmogenic Be-10 Monsoon Record Global Climate Western Tibet Tsangpo River
WOS Research AreaPhysical Geography; Geology
WOS SubjectGeography, Physical; Geosciences, Multidisciplinary ; Physical Geography; Geology
Cooperation Status国内
Citation statistics
Cited Times:3[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8034
Collection图书馆
Corresponding AuthorHu, G
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Bldg 3,Courtyard 16,Lin Cui Rd, Beijing 100101, Peoples R China.
2.Peking Univ, Dept Geog, Key Lab Earth Surface Proc, Beijing 100871, Peoples R China.
3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China.
4.Natl Ctr Accelerator Mass Spectrometry Xian, Shaanxi Prov Key Lab Accelerator Mass Spectrometr, Xian 710061, Shaanxi, Peoples R China.
5.China Univ Geosci, Minist Educ, Key Lab Tecton & Petr Resources, Wuhan 430074, Hubei, Peoples R China.
Recommended Citation
GB/T 7714
Hu, G ,Yi, CL ,Zhang, JF ,et al. Extensive glacial advances during the Last Glacial Maximum near the eastern Himalayan syntaxis[J]. QUATERNARY INTERNATIONAL,2017,443(0):1-12.
APA Hu, G .,Yi, CL .,Zhang, JF .,Dong, GC .,Liu, JH .,...&Hu, G.(2017).Extensive glacial advances during the Last Glacial Maximum near the eastern Himalayan syntaxis.QUATERNARY INTERNATIONAL,443(0),1-12.
MLA Hu, G ,et al."Extensive glacial advances during the Last Glacial Maximum near the eastern Himalayan syntaxis".QUATERNARY INTERNATIONAL 443.0(2017):1-12.
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