The hydrofracturing breccia is formed by deep rich-sodic and gold-hosted fluid hydrofracturing in a set of Devonian system hot-water sedimentary rich-sodic rocks.

• 认为该水压角砾岩体是深源富堿含金流体在泥盆系一套热水沉积的富钠质岩系中发生水力压裂作用形成的。