相山矿田游坊地区地电提取找矿预测

唐瑞, 欧阳菲, 罗先熔, 郑超杰, 汤国栋, 刘攀峰, 蔡叶蕾, 杨笑笑

The prediction of electrochemical prospecting in Youfang area of the Xiangshan orefield

TANG Rui, OUYANG Fei, LUO Xian-Rong, ZHENG Chao-Jie, TANG Guo-Dong, LIU Pan-Feng, CAI Ye-Lei, YANG Xiao-Xiao

图1 相山盆地地质构造略图(据董保平[25]修改) 1—白垩系上统龟峰群;2—白垩系下统鹅湖岭组;3—白垩系下统打鼓顶组;4—三叠系上统安源组;5—石炭系下统华山岭组;6—新元古界;7—次斑状花岗岩;8—花岗岩;9—实测、推测断层;10—赣杭断裂带;11—赣杭构造带范围;12—红色断陷盆地;13—火山盆地;14—铀矿床;15—相山矿田;16—研究区

Fig.1 Outline of geological structure in Xiangshan basin(revised according to Dong Bao-ping[25]) 1—upper Cretaceous Guifeng group; 2—lower Cretaceous Ehuling formation; 3—lower Cretaceous Daguding formation; 4—upper Triassic Anyuan formation; 5—lower Carboniferous Huashanling formation; 6—Neoproterozoic; 7—subporphyritic granite; 8—granite; 9—real and inferred faults; 10—Gan-Hang fault zone; 11—Gan-Hang structural belt range; 12—red fault basin; 13—volcanic basin; 14—uranium deposit; 15—Xiangshan ore field; 16—research area