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《Journal of Geomechanics》 2002-04
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FABRIC ANALYSIS OF GRAVEL IN QUATERNARY GRAVEL BEDS ON BACKBONE AREA OF NIQINGTANGGULASHAN MOUNTAINS

ZHU Da-gang1, ZHAO Xi-tao2,MENG Xian-gang1,WU Zhong-ha1, SHAO Zhao-gang1, FENG Xiang-yang3,WANG Jin1,YANG Chao-bin4 (1.Institute of Geomechanics, CAGS research, Beijing 100081,China; 2. Iinstitute of Geology Geophysics, Academia of Sciences, Beijing 100029,China; 3. National Geological Museum of China, Beijing 100034,China 4. The Land and Resources Department of the Xizang (Tibet) Autonomous Region, Lasa 850000,China.)  
The authors expound the source, the origin and the transport of different original Quaternary gravel beds in south and north of Nianqingtanggoulashan Mountains, from the bedrock strata, the compositional, the granulometric and the psephitic analysis, based on fabric analysis of Quaternary gravel beds on backbone area of Niqingtanggulashan Mountains. It is obvious difference in the rock composition, the grain sizes, the sphericity, the intensity of weathering on the 3 Gravel Beds of glacial epoch phases in the middle section of Nianqingtanggoulashan Mountains. This difference reflecs the denudation of the different rocks of Nianqingtanggoulashan Mountains in the doming of Qinghai-Xizang (Tibet) plateau.
【Fund】: 国土资源大调查项目“西藏纳木错地区第四纪环境演变调查研究” (编号 :DKD2 0 0 10 0 6 );; “西藏当雄幅 1∶2 5万区域地质调查” (编号 :DKD990 10 0 1)
【CateGory Index】: P534.63
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