Extensive glacial advances during the Last Glacial Maximum near the eastern Himalayan syntaxis
文献类型:期刊论文
作者 | 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 |
刊名 | QUATERNARY INTERNATIONAL |
出版日期 | 2017 |
卷号 | 443期号:0页码:1-12 |
关键词 | Southeastern Tibetan Plateau Late Quaternary Glaciations Equilibrium-line Altitudes Regenerative-dose Protocol Late Pleistocene Cosmogenic Be-10 Monsoon Record Global Climate Western Tibet Tsangpo River |
DOI | 10.1016/j.quaint.2016.08.005 |
文献子类 | Article |
英文摘要 | Climatically, 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. |
学科主题 | 自然地理学 |
WOS研究方向 | Physical Geography; Geology |
语种 | 英语 |
WOS记录号 | WOS:000406753900001 |
源URL | [http://ir.itpcas.ac.cn/handle/131C11/8034] |
专题 | 青藏高原研究所_图书馆 |
通讯作者 | Hu, G |
作者单位 | 1.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. |
推荐引用方式 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. |
入库方式: OAI收割
来源:青藏高原研究所
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。