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万山类型汞矿床主要分布在貴州高原的东北部。該区地形切割非常剧烈。所述之呈北北东向带状产出的矿体,其区域构造为江南古陆的边緣部分(据黄汲清)。由于矿区內岩石几乎呈水平状,因此区內构造相对簡单。区內整合类型(似层状)矿体一般均赋存在中、下寒武紀不同岩性的有利层位中,而且主要是赋存在条带状白云岩中(与碳酸岩相比,白云岩自行充填裂隙的性能較差),並受剝离构造控制。遮挡作用較为次
Wanshan type mercury deposits are mainly distributed in the northeast of Guizhou Plateau. Terrain cutting the area is very intense. According to the ore body emerging from the north-easterly belt, the region is constructed as the marginal part of the ancient Jiangnan land (according to Huang Jiqing). Since the rocks in the mining area are almost horizontal, the structure in the area is relatively simple. Generally, the intracontinental type (stratiform) orebodies are found in the favorable lithofacies of different lithologies in the Middle and Lower Cambrian, and are mainly present in banded dolomites (compared with carbonate rocks, Fissure filling performance is poor), and controlled by the stripping structure. Blocking effect is more times