多维度化探异常研究在黔西南者相金矿床深部成矿预测中的应用

邰文星, 杨成富, 靳晓野, 邵云彬, 刘光富, 赵平, 王泽鹏, 谭礼金

Application of the multi-dimensional study of geochemical anomalies in deep metallogenic prediction of the Zhexiang gold deposit in southwestern Guizhou, China

TAI Wen-Xing, YANG Cheng-Fu, JIN Xiao-Ye, SHAO Yun-Bin, LIU Guang-Fu, ZHAO Ping, WANG Ze-Peng, TAN Li-Jin

图1 黔西南灰家堡背斜矿田分布(a)及者相金矿区地质(b)(按文献[3]修编) 1—第四系浮土;2—三叠系嘉陵江组第一段二亚段黏土岩;3—三叠系嘉陵江组第一段一亚段白云岩夹灰岩;4—三叠系夜郎组第三段钙质黏土岩;5—三叠系夜郎组第二段生物碎屑灰岩;6—正断层; 7—逆断层;8—背斜;9—金矿床;10—勘查线

Fig.1 Distribution of Huijiapu anticline ore field (a) and geology of Zhexiang gold deposit (b) in southwest of Guizhou Province(revised according to reference [3]) 1—Quaternary floating soil;2—clay rocks of the second sub-member of the first member of Jialingjiang formation of Triassic system;3—dolomite limestone of the first sub-member of the first member of Jialingjiang formation of Triassic system;4—calcareous clay rocks of the third member of the Yelang formation of Triassic system;5—bioclastic limestone of the second member of the Yelang formation of Triassic system;6—normal fault;7—thrust fault;8—anticline;9—gold deposit;10—line of survey