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浊积岩型金矿是指产在浊积岩中的受背斜和断层控制的含金石英脉。这种浊积岩受到绿片岩相变质作用,并经历造山运动形成了许多褶皱和断层。同时有花岗岩侵入。含金石英脉是在浊积岩,造山运动和变质作用之后形成的。主要分布于背斜的轴部和两翼,且平行于地层(Bed Parallele vein;BPV)。
Turbidite-type gold deposits are gold-bearing quartz veins controlled by anticlines and faults in turbidites. This turbidite is subjected to greenschist facies metamorphism and is subjected to orogeny to form many folds and faults. Granite intrusion at the same time. Gold-bearing quartz veins are formed after turbidites, orogeny and metamorphism. Mainly distributed in the anticline shaft and wings, and parallel to the bed (Bed Parallele vein; BPV).