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。
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.
出处
《干旱区地理》
CSCD
北大核心
2001年第2期104-108,共5页
Arid Land Geography
基金
国家自然科学基金 (498610 0 5 )
日本本部省科学基金
国家重点基础研究 (G19990 43 5 0 8)资助项目&&
关键词
空间分布
冰川
动力过程
天山
spatial distrbutiion, glacier
dynamic process, Tianshan Mountains.