It is one of the effective methods for detecting position of slip plane, measuring thickness of slidebody, finding slip direction, calculating slipspeed and judging deep deformation case of slidebody.
是测定滑坡体滑动面（带）位置、滑体厚度、滑动方向、滑速及判断滑体深部变形状态行之有效的方法之一。
Mann equates the fault in Haiti with the San Andreas fault in California, as both have plates that slip and grind past one another in a horizontal direction.
曼认为海地的断层与加利福尼亚圣安地列斯的断层是相似的，因为两者的板块都在朝地平线的方向相互滑动研磨。
An adiabatic shear band formed along the main shear stress around the penetrated hole is approximately consistent with the direction of plastic deformation slip lines in static state.
弹孔周围的绝热剪切带沿主剪应力方向形成，与静态塑性变形滑移线方向接近，绝热剪切带上不均匀的变形将产生微裂纹和微孔洞。
The life is like a slip on the open ocean, the goal is like a beacon, which gives us the direction of going.
生活就像茫茫大海中的一只小船，而目标就像一个灯塔，它给了我们前进的方向。
The combination of a crystallographic plane and, within that plane, a crystallographic direction along which slip (i. e. , dislocation motion) occurs.
滑移面和该面上一个滑移方向的组合称为一个滑移系，晶体滑移（如位错的移动）可以沿该系统发生。
We must pay attention to the linear landforms when we determine direction and displacement amount of strike-slip fault.
判读走滑断层的变位方向及变位量，需注意地貌面上的线性地物。
In Longling fault zone and the area north to it, the direction of maximum compressional stress is near NS or NNW, the stress regime is of strike slip type.
龙陵断裂带及其以北的局部地区，最大主压应力方向为近南北或北北西，应力结构为走滑型。
Faults which move along the direction of the dip plane are dip-slip faults and described as either normal or reverse, depending on their motion.
沿倾角方向移动的断层称为倾滑断层，并按他们的运动方向分别描述为正向或逆向。
The fore-body with sharp section angle can produce direction stability at middle-higher angle of attack in the case of side-slip.
有侧滑时，尖侧缘的非圆截面机身头部在中等和大迎角下，可具有方向稳定性。
The observations of seismologists at the BGS suggest both things: more thrust in the SW, nearer the epicentre, and more strike-slip toward its direction of propagation, the NE.
地震学家在BGS上的观测暗示出两件事：在接近于震源中心部位的西南方向上有更大的推力；在东北方向的传播方位上有更大的碰撞滑动。
The observations of seismologists at the BGS suggest both things: more thrust in the SW, nearer the epicentre, and more strike-slip toward its direction of propagation, the NE.
地震学家在BGS上的观测暗示出两件事：在接近于震源中心部位的西南方向上有更大的推力；在东北方向的传播方位上有更大的碰撞滑动。
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