oblique strike-slip faults 斜走向滑断层
dip-slip faults 倾斜滑动断层
dip slip faults 倾斜滑动断层
flexural-slip faults 弯滑断层
Insidious strike-slip faults 隐伏走滑断裂
large-sized strike slip faults 大型走滑断裂
slip sheeting faults 层滑断裂
The foreland thrust belt has complex and various structural styles. Besides the large-scale reverse faults, there are a series of north-west strike-slip faults.
准噶尔盆地西北缘前陆冲断带构造样式复杂多样，除规模较大的逆断层外，还发育一系列北西向的走滑断层。
The strata form and quasi strata form ore bodies are controlled by strike slip faults.
矿体受层滑断层控制呈层状、似层状。
The formation time of NE strike slip faults is earlier than that of NW strike slip faults.
另一组为NW向走滑断层，形成时代较晚，破坏早期逆冲断层和NE向走滑断层。
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