青藏高原腹地各拉丹冬南北坡多年冻土考察初步结果
|
刘广岳 1,2( ), 邹德富 1, 杨斌 3, 杜二计 1,2, 周华云 1,2, 肖瑶 1, 赵林 2,4( ), 谭昌海 3, 胡国杰 1, 庞强强 1, 王武 1, 孙哲 1,2, 朱小凡 1, 殷秀峰 1, 汪凌霄 4, 李智斌 4, 谢昌卫 1
|
Preliminary results of permafrost investigation on northern and southern slopes of Mt. Geladandong, interior Qinghai-Tibet Plateau
|
Guangyue LIU 1,2( ), Defu ZOU 1, Bin YANG 3, Erji DU 1,2, Huayun ZHOU 1,2, Yao XIAO 1, Lin ZHAO 2,4( ), Changhai TAN 3, Guojie HU 1, Qiangqiang PANG 1, Wu WANG 1, Zhe SUN 1,2, Xiaofan ZHU 1, Xiufeng YIN 1, Lingxiao WANG 4, Zhibin LI 4, Changwei XIE 1
|
|
图3. 扎加藏布源区和沱沱河源区的典型冰缘地貌
|
Fig. 3. Several kinds of typical periglacial landforms discovered in source area of the Zhaga Zangbo River and source area of the Tuotuo River: a rock glacier (a), weathered bedrock and kurums (debris slope) (b), a small cirque glacier (c), debris slope (d), polygon soil (e), thermokast lakes and pingos (f), retrogressive thaw slump (g) and a perennial pingo (h) (The photos were taken on November 10, 2020, and the white dot marks the location of borehole dilled at the top of pingo)
|
|
|
|
|