激发极化法在覆盖区矿产勘查中的应用——以内蒙古昌图锡力锰银铅锌多金属矿勘查为例

马一行, 颜廷杰, 何鹏, 刘祖鉴, 苏航, 郭硕

Exploration in coverage area: A case study of the Changtuxili Mn-Ag-Pb-Zn polymetallic ore deposit,Inner Mongolia

Yi-Xing MA, Ting-Jie YAN, Peng HE, Zu-Jian LIU, Hang SU, Shuo GUO

图1 昌图锡力地区地质简图 1—全新统冲积层;2—全新统冲洪积层;3—全新统湖积层;4—上新统宝格达乌拉组;5—下白垩统白音高老组;6—上侏罗统玛尼吐组;7—流纹岩脉;8—安山玢岩脉;9—地质界线;10—断层;11—火山口;12—火山断层;13—矿化带及编号;14—激电测量范围;15—钻孔及编号

Fig.1 Geological map of the Changtuxili area in Inner Mongolia 1—Holocene Alluvium;2—Holocene Diluvium;3—Holocene Lacustine Deposit;4—Baogedawula Formation of Upper Miocene;5—Baiyingaolao Formation of Lower Cretaceous;6—Manitu Formation of Upper Jurassic;7—rhyolite vein;8—andesitic porphyrite vein;9—geological boundary;10—fault;11—volcanic vent;12—volcanic fault;13—mineralized zone and number;14—IP measuring range;15—drill hole and number