Strike-slip faults occurring in the converging crust, or transpression, rocks are faulted upward in a positive flower structure.
在会聚的地壳或压转岩石中发生的走滑断层以正花构造向上断裂。
Thrust- faults and strike-slip faults are the major structures in the studied area.
逆冲断层及边界走精断层是区内主要控矿构造。
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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