Thaw slumping existing on two slopes in the permafrost region of Qinghai-Tibet Plateau are studied with their geological, frozen soil conditions and deformations.
以发育于青藏高原多年冻土区平缓斜坡上的两处热融滑塌为例 ，研究了热融滑塌发育的斜坡地质、冻土条件及变形特征。
Thaw slumping existing on two slopes in the permafrost region of Qinghai-Tibet Plateau are studied with their geological, frozen soil conditions and deformations.
以发育于青藏高原多年冻土区平缓斜坡上的两处热融滑塌为例 ，研究了热融滑塌发育的斜坡地质、冻土条件及变形特征。
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