锦屏山
- 网络Jinping Mountain
锦屏山-
锦屏山裂隙岩体的渗透系数的空间非均质分布利用随机连续模型生成。
The spatial uneven distribution of the seepage coefficient of the fractured rock mass in Jinping Mountain was produced by the stochastic continuum model .
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锦屏山地区推覆构造带滑移面均为韧性剪切带，而且整个推覆构造带由多个岩片推覆堆叠在一起，在其前缘则出现飞来峰群。
The nappe structures in this area are generally overthrusted and stacked by a number of slices and sheets , with thrust outliers in the front of the nappe structures .