Maoduqing gold deposit occurred in the green schist and marble stratum belt of paleoprotozoic Inner Mongolia.

卯独庆金矿床赋存在古元古代二道凹岩群的绿片岩层与大理岩层过渡带.

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The host rocks of Dashuigou independent tellurium ore deposit are mainly green schist facies metamorphic rocks.

大水沟独立碲矿床的直接赋矿围岩为低绿片岩相变质岩.

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The rocks from the Group Complex have been highly metamorphosed into the green schist facies.

该群岩石变形非常强烈,变质达绿片岩相.

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