ARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>ana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>Glacial Advance in the Qinghai-Tibet Plateau and amespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />
- 责任者：Wang Jie (Key Laboratory of Western China’s Environmental Systems ; Ministry of Education ; Lanzhou University ; Lanzhou730000 ; China)
- 刊名：Quaternary Sciences
- 出版年：2010
- 卷期：30(5)
- 关键词：第四纪 ; Quaternary ; 冰川作用 ; glaciation ; 冰期 ; glacial stage ; 青藏高原 ; Qinghai-Tibetan Plateau
- 页码：p.1055-1065
- 索书号：P515.206/633-4
- 图表：3 illus., 1 table, 67 refs.
- 分类号：1400
- issnNo：ISSN1001-7410
- isbnNo：CN11-2708/P
ang=EN-US>The paper reviewed dating results in the Tibetan Plateau and peripheral mountains. The studies show that the local last glacial maximum (LGML) in Himalaya and the south eastern Tibetan Plateau occurred in MIS 3 (58～ang=EN-US>32 ka B.P.) (especial in Mid-MIS 3 or 54～ang=EN-US>44 ka B.P.) rather than in the global Last Glacial Maximum (LGMG or 25～ang=EN-US>15 ka B.P.) of MIS 2. Moreover, MIS 3 glacial advances happened in about 30 areas in Central Asia, including Hindu Kush Mountains, Himalaya Mountains, Kunlun Mountains, Nyainqêntanglha Mountains, Tanggula Mountains, Karakorum Mountains, Hengduan Mountains, Qilian Mountains, Tianshan Range, Pamir Plateau, and high mountains of Taiwan.