岩脉的分布受断层构造的控制，刘家沟石英闪长岩体的展布特点说明其就位受近南北向和北西向断层的控制。
The characteristic of quartz-diorite in Liujiagou shows that it is controlled by the compound positions of the north-west striking and north-south striking faults.
山西省昔阳县境内寺家庄井田在构造上处于阳泉矿区地层走向由北西向南北方向的转折地带，先后经过三次应力作用。
The Sijiazhuang minefield in Xiyang County, Shanxi Province is located in the Yangquan mining area strike transition from NW to NS zone, had experienced three stressing actions early or late.
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。
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.
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