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。

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The middle member is the gravity slide collapse block and breccia facies-structural movement type alluvial fan facies sediments.

中段为重力滑塌岩块及角砾岩相-构造活动型冲积扇相沉积；

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