构造原生晕在攻深找盲中的应用——以赣南银坑牛形坝铅锌金银矿床为例

陈伟, 谭友, 曹正端, 廖志权, 张宁发, 傅海晖

Application of tectonic primary halos in the exploration of deep concealed ore bodies: A case study of the Niuxingba plumbum-zinc-gold-silver deposit in Yinkeng, southern Jiangxi

CHEN Wei, TAN You, CAO Zheng-Duan, LIAO Zhi-Quan, ZHANG Ning-Fa, FU Hai-Hui

图3 银坑牛形坝矿区近东西向脉状矿带(体)A-A'综合地质剖面 1—侏罗系中统罗坳组;2—青白口系上统库里组;3—泥岩、细砂岩;4—板岩、变凝灰岩;5—花岗斑岩;6—石英斑岩;7—花岗闪长斑岩;8—矿带(体)及编号;9—断裂及编号;10—坑道;11—钻孔

Fig.3 Comprehensive geological profile of east-west nearly vein-type ore belt (body)in Niuxingba mining area, Yinkeng 1—middle Jurassic Luo'ao formation;2—upper Qingbaikou system Kuli formation;3—mudstone,fine sandstone;4—slate,metatuff;5—granite porphyry;6—quartz porphyry;7—granodiorite-porphyry;8—ore zone (body) and number;9—fracture and number;10—gallery;11—borehole