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《Journal of Glaciology and Geocryology》 1989-03
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Function of Geologic Structure in the Formation of Permafrost Conditions in Huola River Basin, North Da Hinggan Ling

Guo Dongxin et al. (Lanzhou Institute of Glaciologv and Geocryology, Chinese Academy of Sciences)  
Huola river is located in the north Da Hinggan Ling, and its geographical coordinate ranges from lat. 52°27 '-53°03 ' and long. 121°52 ' -122°04 ' administratively, this area belongs to Mohe County of Heilongjiang Province. The features of permafrost in the Basin are that from the centre to the margin of the Basin, the thickness of permafrost becomes thinner, from 100-120 m to 10-20 m, and the mean annual ground temperature gets higher, from -2.9℃ to 0.5℃ . Talik occurs on the surrounding mountains only. Geologic structure controls the topography, facies and the distribution of rocks. Because of the differences of development processes, tectonic activity patterns and external agents between the surrounding mountains and the Basin, geologic structure, sendimentary facies, lithology, development degree of fissures and motive regularities of ground water also vary greatly from place to place. These variations play an important part in the formation of permafrost conditions in the Basin.
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