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Arid Land Geography ›› 2001, Vol. 24 ›› Issue (2): 104-108.doi: 10.13826/j.cnki.cn65-1103/x.2001.02.002

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SPATIAL DISTRIBUTION CHARACTERISTICS OF GLACIAL-DYNAMIC PROCESS IN THE TIANSHAN MOUNTAINS, XINJIANG

XIONG Hei-gang1, TASHPOLAT Tiyip1, ZHONG Wei1, SUN Lin1, NUERBAYI Haimiti1, Hiroki TAKAMURA2, Yuichi Suzuki2   

  1. 1. Department of Resources, Envirionment and Information Science, Xinjiang University, Urumqi 830046, China;
    2. Faculty of Geo-Environmental Science, Rissho University, Japan
  • Received:2000-10-18 Revised:2001-03-12 Published:2025-12-31
  • Supported by:
    Natural Science Foundation of China, No.49861005:Science Foundation of Education Ministry, Japan and Base Project of China, No.G1999043508

Abstract: The dynamic procss in glacial environment is characterized multiple types and complexity, Grenerally the squeeze and abrasion processes develop at the glacial sole, and the processes of slope, slide-deposition, drop-deposition, feuvial process, freezing-weathering, etc. occur at other places. The former can really reflect the nature of the glacial dynamic process. In all the landform processes (erosion, transport and depostion), the deposition process controls the structure, stratigraphic succession, fabric and facies models of tiee.

Key words: spatial distrbutiion, glacier, dynamic process, Tianshan Mountains

CLC Number: 

  • P343.6