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干旱区地理 ›› 2001, Vol. 24 ›› Issue (2): 104-108.doi: 10.13826/j.cnki.cn65-1103/x.2001.02.002

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新疆天山冰川区动力过程的空间分布特征

熊黑钢1, 塔西甫拉提1, 钟巍1, 孙林1, 努尔拜依1, 海米提1, 高村弘毅2, 铃木裕一2   

  1. 1.新疆大学资源环境信息科学系, 乌鲁木齐 830046;
    2.日本立正大学地球环境科学部
  • 收稿日期:2000-10-18 修回日期:2001-03-12 发布日期:2025-12-31
  • 基金资助:
    国家自然科学基金(49861005)和日本本部省科学基金和国家重点基础研究(G1999043508)资助项目&&

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 Online: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

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摘要： 冰川环境中的动力过程种类多且复杂。一般冰底以挤压、磨蚀等过程为主, 其它部位则是以斜坡、塌积、坠落、流水、寒冻风化等过程最多。前者能真正反映冰川动力过程的本质。地貌全过程(侵蚀、搬运、堆积)中, 堆积过程控制着冰碛的构造、层序、组构和相模式。

关键词: 空间分布, 冰川, 动力过程, 天山

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

中图分类号: 

  • P343.6