走向滑动断层(strike slip fault)是指相对位移方向与断层走向平行的断层。根据观察者面向的对盘错移方向可描述为左行走向滑动断层和右行走向滑动断层。过去的地质文献中曾出现许多同义异名词,如平移断层(transcurrent fault)、平推断层、横推断层(transverse fault)、挫断层(wrench fault)、平挫断层等;它们各自的涵义有的相同,大多又略有区别或大同小异,各用于特定的场合和不同的地质条件。
... strike-shift fault 平移断层 strike-slip fault 走向滑动断层 strike-slip microfault 走向滑动微断层 ...
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作为该方法的应用实例。本文对直立走向滑动断层的水平、垂直位移场及倾斜、应变场进行了模拟计算。
As an example of this method, the horizontal and vertical displacement field and the tilt and strain field due to vertical strike faulting are calculated.
给出了半无限空间中任意倾角的走向滑动剪切断层错动产生的应力场的一套严密的解析表达式。
A complete suit of closely analytical expressions of stress field is presented for the strike slip shear fault with an arbitrary dip Angle in a semi infinite medium.
由此推测,主震的错动面为北西西走向,可能是高倾角的左旋平移断层的滑动结果。
From this, it has been inferred that the strike of the dislocating fault plane of the main shock is NWW. It seems to be a left lateral horizontal slip fault with high dipping Angle.
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