• 责任者：Wang Chengshan (State Key Laboratory of Geological Processes and Mineral Resources ; School of Earth Sciences and Resources ; Research Center for Tibetan Plateau Geology ; China University of Geosciences ; Beijing 100083 ; China) ; Dai Jingen
• 刊名：Earth Science Frontiers
• 出版年：2009
• 卷期：16(3)
• 关键词：隆起 ; uplifts ; 喜马拉雅山 ; Himalayas
• 页码：p.1-30
• 图表：7 illus., 4 tables, 225 refs.
• 分类号：0300
• issnNo：ISSN1005-2321
• isbnNo：CN11-3370/P

The uplift history of Tibetan Plateau and oft-com:office:smarttags" />Himalaya is the key boundary condition in many Cenozoic geological events. On the basis of the studies in north-central Tibet, as well as the existing possible estimates, the authors provide a new model for the growth of Tibetan Plateau: Lhasa and Qiangtang terranes gained their elevations during Eocene time, whereas its northern area was still low and southern area was under sea level at that time. The Proto-Tibetan Plateau expanded throughout the Neogene toward its present southern and northern margins in the Himalaya and Qilian Mountains.  oft-com:office:office" />