四川大梁子铅锌矿床1 944 m中段构造岩元素组合异常及隐伏矿体预测
王海丰1(
),龚红胜2(),冯志兴1,韩润生2,丁天柱3,赵新跃3,吴鹏2
),龚红胜2(),冯志兴1,韩润生2,丁天柱3,赵新跃3,吴鹏2
Element Association Anomalies of Tectonite and Prediction of Concealed Orebodies in the 1 944 m Middle Section of Daliangzi Pb-Zn Deposit，Sichuan
Haifeng WANG1(),Hongsheng GONG2(),Zhixing FENG1,Runsheng HAN2,Tianzhu DING3,Xinyue ZHAO3,Peng WU2
),Hongsheng GONG2(),Zhixing FENG1,Runsheng HAN2,Tianzhu DING3,Xinyue ZHAO3,Peng WU2
图1. 川滇黔铅锌成矿区主要断裂及矿床分布图（据
1.超大型、大型铅锌矿床；2.中、小型铅锌矿床；3.城镇；4.省界；5.金沙江及流向；6.构造带及编号；7.断裂；8.峨眉山玄武岩；9.本次工作区范围；a-安宁河断裂带；b-小江断裂带；c-康定—彝良—水城断裂带；d-弥勒—师宗断裂带；e-昭通—曲靖断裂带；f-寻甸—宣威构造带；g-矿山厂—金牛厂构造带；h-会泽—彝良构造带；i-巧家—大关构造带；j-巧家—金沙厂构造带；k-普渡河断裂带
Fig.1. Distribution map of main faults and deposits in the Sichuan-Yunnan-Guizhou lead-zinc metallogenic area （modified after
