首页 | 本学科首页   官方微博 | 高级检索  
     


Palaeoglaciation of Bayan Har Shan,northeastern Tibetan Plateau: glacial geology indicates maximum extents limited to ice cap and ice field scales
Authors:Jakob Heyman  Arjen P. Stroeven  Helena Alexanderson  Clas Hättestrand  Jon Harbor  Yingkui Li  Marc W. Caffee  Liping Zhou  Daniel Veres  Feng Liu  Martin Machiedo
Affiliation:1. Department of Physical Geography and Quaternary Geology, Stockholm University, Sweden;2. Department of Plant and Environmental Sciences, Norwegian University of Life Sciences, ?s, Norway;3. Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana, USA;4. Department of Geography, University of Tennessee, Knoxville, Tennessee, USA;5. Department of Physics, Purdue Rare Isotope Measurement Laboratory, Purdue University, West Lafayette, Indiana, USA;6. Department of Geography, Peking University, Beijing, China;7. ‘Emil Racovita’ Institute of Speleology, Cluj, Romania;8. Department of Geology, University Centre in Svalbard (UNIS), Svalbard, Norway
Abstract:Key locations within an extensive area of the northeastern Tibetan Plateau, centred on Bayan Har Shan, have been mapped to distinguish glacial from non‐glacial deposits. Prior work suggests palaeo‐glaciers ranging from valley glaciers and local ice caps in the highest mountains to a regional or even plateau‐scale ice sheet. New field data show that glacial deposits are abundant in high mountain areas in association with large‐scale glacial landforms. In addition, glacial deposits are present in several locations outside areas with distinct glacial erosional landforms, indicating that the most extensive palaeo‐glaciers had little geomorphological impact on the landscape towards their margins. The glacial geological record does indicate extensive maximum glaciation, with local ice caps covering entire elevated mountain areas. However, absence of glacial traces in intervening lower‐lying plateau areas suggests that local ice caps did not merge to form a regional ice sheet on the northeastern Tibetan Plateau around Bayan Har Shan. No evidence exists for past ice sheet glaciation. Copyright © 2009 John Wiley & Sons, Ltd.
Keywords:glacial deposits  Tibetan Plateau  Bayan Har  glacial extent  palaeoglaciology
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号