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1地质概况盘龙铅锌矿床位于广西武宣县。构造位置属于华南陆缘构造区桂中—桂东边缘海的柳州—桂林被动陆缘区,处于桂中武宣—象州铅锌金属成矿带的南段。矿区出露地层有寒武系、泥盆系、石炭系、二叠系和第四系,寒武系和泥盆系下统莲花山、高岭组岩性为碎屑岩,泥盆系下统上伦组、官桥组和中泥盆系东岗岭组及上泥盆系融县组及榴江组均为碳酸盐岩。矿体主要赋存
1 Geological Survey Panlong lead-zinc deposit is located in Guangxi Wuxuan County. It is located in the Liuzhou-Guilin passive margin region of the Guizhong-Guidong marginal sea in the southern China continental marginal zone and is located in the southern section of the Wuxuan-Xiangzhou Pb-Zn metallogenic belt in the Central Guangxi. There are Cambrian, Devonian, Carboniferous, Permian and Quaternary, Cambrian and Devonian lower Lianhuashan and Gaoling lithologies of clastic rocks and Devonian strata The Tongshanglun, Guanqiao and Middle Devonian Donggangling formations and the Upper Devonian Rongxian Formation and the Jujiang Formation are all carbonate rocks. The main ore body