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清镇铝土矿位于扬子准地台之贵阳复杂构造变形区的西端北东向构造带中,区域性猫山断层的西盘,河口背斜之南东翼。矿区含矿地层为石炭系下统九架炉组(C1jj),赋存于寒武系中上统娄山关群(∈2-3 1s)白云岩侵蚀面之上、二叠系中统梁山组(P2l)灰色、灰黄色粉砂质页岩之下。长期以来,众多专家学者对贵州铝土矿进行了大量的研究,如铝土矿的矿床特征、地球化学特征、物质来源、矿床学特征及成矿机制,取得了大量的研究成果,但对于铝土矿的矿物学特征,特别是黔中地区的铝土矿的矿物学特征仍较欠
Qingzhen bauxite is located in the north-eastward structural belt of the western end of the Guiyang complex structural deformation zone of the Yangtze quasi-platform, the western plate of the regional Cathayan fault and the southern wing of the estuary anticline. The ore-bearing strata are the Lower Carboniferous 9 coal-bearing formations (C1jj) that occur on the eroded surface of the dolomite of the middle Cambrian Loushanguan Group (∈2-3 1s) in the Cambrian, Group (P2l) gray, grayish silty shale. For a long time, many experts and scholars have conducted a great deal of research on Guizhou bauxite, such as the deposit features, geochemical characteristics, material sources, mineralization features and mineralization mechanisms of bauxite. A great deal of research results have been obtained. However, The mineralogical characteristics of earth mines, especially the mineralogical characteristics of bauxite in central Guizhou are still less than