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《Hydrogeology and Engineering Geology》 1990-01
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Wang Shaoling  
Field investigation and indoov experiments havediscovered from the island permafrost areas in Qin-ghai-Xizang (Tibet) plateau the "high-temperature"unsaturated coarse-grained soil (rock)layers of aver-age annual temperature above-0.5℃ Which ate ca-pable of both water permeation and water releasing.They belong to a special kind of aquifer whosewater is called "intrapermafrost water" .
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