The studies of organic geochemistry on the ore-bearing formation show that the host-rock is rich in primary organic matters and the sedimentary environment is low basin in the epicontinental sea.
含矿建造的有机地球化学研究表明:主岩富含原生有机质,其沉积环境为还原一强还原的浅海低洼海盆。
The host rocks of the ore bodies, the Gaixian Formation of Liaohe Group, are a medium grade metamorphosed rock of the Early Proterogoic.
矿体围岩为早元古界辽河群盖县组中部变质岩系。
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