贵州铝厂清镇林歹矿床属龙头山背斜的西异,走向近南北,倾向东。先建设的Ⅰ号矿体,为品位高、产状较稳定、急倾斜薄的铝土矿体。倾角65°～80°,厚度1～8米,走向长1000米,延深400米,上宽下窄逐渐尖灭。矿体呈透镜状或薄饼状,但膨缩变化较大,加之横向小断裂发育,连续性较差。 Guizhou Aluminum Plant Qingzhen Linruan deposit belongs to the west divergence of the Longtoushan anticline, and tends toward the north and south and tends to the east. The No. 1 orebody that was first constructed is a bauxite ore body with high grade, stable shape and thin inclination. Inclination 65 ° ~ 80 °, the thickness of 1 to 8 meters, to the long 1000 meters, 400 meters deep, wide and narrow gradually narrowed. Ore was lenticular or pancake shape, but the larger changes in swelling, combined with the development of small transverse rupture, poor continuity.