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渔塘铅锌矿床产于寒武纪碳酸盐岩中,主要受构造、岩性和藻礁相控制。 由于铜渔驻同生断裂带的活动,幔源铅锌沉积在下寒武统清虚洞组藻礁内,形成矿源层。在加里东末期的构造运动中,主要是构压溶液成矿,主要产生整合型矿体。强烈的地洼拱裂运动,先者的矿床被叠加富化,主要以脉状矿体赋存为特征。 成矿作用可分为地台和地洼两个阶段。二者均有两个成矿期。很明显,矿床具有多成矿阶段、多物质来源、多成因的三多特点。其类型应属多因复成矿床。
Yuetang lead-zinc deposits are produced in Cambrian carbonate rocks and are mainly controlled by tectonics, lithology and algal reefs. Due to the activity of copper fishing in the Tongsheng fault zone, the lead-zinc mantle plunged into the Algae and Reef within the Lower Cambrian Qingxuendong Formation to form a source layer. During the Caledonian tectonic movement, the solution mineralization mainly resulted from the formation of an integrated ore body. Intense pothole arch-splitting movement, the first deposit is superimposed and enriched, mainly to the presence of vein ore body is characterized. Mineralization can be divided into platform and depression two stages. Both have two mineralization stages. Obviously, the deposit has multi-mineralization stage, multi-material source, multi-cause more than three features. Its type should be due to multiple gold deposits.