层间滑动角砾岩型金矿在盆地的长期演化过程中形成，经历了从伸展—挤压—走滑的构造环境。
The interlayer slide breccia type gold deposit was resulted from a secular evolution of the basin, which had experienced extension, compression and slip.
层间滑动角砾岩型金矿在盆地的长期演化过程中形成，经历了从伸展—挤压—走滑的构造环境。
The interlayer slide breccia type gold deposit was resulted from a secular evolution of the basin, which had experienced extension, compression and slip.
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