青藏高原腹地各拉丹冬南北坡多年冻土考察初步结果
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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
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Preliminary results of permafrost investigation on northern and southern slopes of Mt. Geladandong, interior Qinghai-Tibet Plateau
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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
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图6. 沱沱河源区不同类型的泉水
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Fig. 6. Different kinds of springs in source area of the Tuotuo River: a hot spring with outlet water temperature above 55 ℃ (a), travertines at the mouth of a hot spring (b), a small hot spring on the left bank of the upper Tuotuo River (c) and a small cold spring flowing out of gravels at the foot of slope (d)
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