The gold metallogeny is characterized by auriferous pyrite and occurred in the alternating layer of heavy-layer metasandstone,flaggy metasandstone and graphitization schist.
以含黄铁为特征,产出于盖县组变质
岩段厚层状变质岩、薄层状变质岩和石墨片岩的
层带中,体产状与地层一致;
床成因论The gold metallogeny is characterized by auriferous pyrite and occurred in the alternating layer of heavy-layer metasandstone,flaggy metasandstone and graphitization schist.
以含黄铁为特征,产出于盖县组变质岩段厚层状变质岩、薄层状变质岩和石墨片岩的层带中,体产状与地层一致;
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