1.
Essentials of the Excavation and Monitoring for Twin Closely-spaced Tunnels Embedded in Slidding Rock
穿越易滑岩层小净距隧道开挖与量测控制要点
2.
And the characteristics of homogeneous loess landslide and loess-mudstone cutting layer landslide are high sliding velocity, long sliding distance and high stability after sliding except its scarp.
黄土层内滑坡、土泥岩切层滑坡的滑速高、滑距长,滑体稳定性高。但后壁不稳定,易再次滑动。
3.
As the plates diverge from a mid-ocean ridge they slide on a more yielding layer at the base of the lithosphere.
当板块从中海脊脱离时，它们滑向在岩石圈基部较易变形的地层上。
4.
The Dengying formation encluded carbonate turbidite and gravity sliding layer.
灯影组发育碳酸盐岩浊积岩层和重力滑动层。
5.
A rock formation that resembles beads, found in glassy igneous rocks.
珍珠云母一种存在于光滑的火成岩岩层中的呈珠粒状的岩层
6.
some thin beds of layered sandstone and dark grey siltstone show slump structures.
一些薄层砂岩和暗灰色粉砂岩显示出滑动构造。
7.
Research on Bedding Landslide Form K28 to K32 of the Changzhi to Jincheng Express Highway;
长晋高速公路K28～K32顺层岩质滑坡研究
8.
The characteristics of loess interface landslide and loess-mudstone layer plane landslide are low sliding velocity, short sliding distance and low stability after sliding.
黄土接触面滑坡、土泥岩顺层滑坡的滑速低、滑距短,滑体具有稳定性差、活性强的特点。
9.
The deep-seated weak layer S1 under the slope may lead deep sliding.
场区斜坡三面临空，岩层顺坡向，浅层滑坡体发育，深部分布有S1软弱层，存在著深层滑移问题。
10.
Some Problems Related to the Stability Analysis of a Dam on Layered Rock Foundation
层状岩体坝基抗滑稳定分析中的几个问题
11.
Research on the Caculation Method of Bearing Capacity of Anti-Slide Pile in Xigeda Rock;
昔格达岩层中抗滑桩的承载力计算方法研究
12.
Research on Rockburst Mechanism Induced by Fault Slip during Coal Mining Operation
采动影响下断层滑移诱发煤岩冲击机理研究
13.
Analysis and Treatment of the Cross-bedding Rock Landslide in Xiaojiabao,Chongqing City
重庆市肖家包切层岩石滑坡分析与治理
14.
Stress builds up in the rock on both sides of the fault and causes the rock to break and shift in an earthquake.
压力在断层两侧的岩石中产生，并且引起岩石在地震中破裂和滑动。
15.
Rheological Experimental Study and Mechanism Research on Gentle-dipped Landslides of Jurassic Red Strata in Wanzhou City;
万州区红层岩土流变特性及近水平地层滑坡成因机理研究
16.
The cycle repeated over and over again, building up a series of crusty, crumbly layers.
这样的循环一次次重复，形成了一层层硬且易碎的岩层。
17.
If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.
如果断层上盘和下盘的岩石相对位移运动是平行断层面走向的，这种断层称为走滑断层。
18.
The wall is, also here, commonly talcose, and the beds of phyllite are cut and dragged by the movements.
墙壁，这里也是，一般是滑石化的，千枚岩层被运动所切割、拖曳。