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2. 大梁子铅锌矿区域构造纲要图
N-Q-第三系—第四系；T-K-三叠系—白垩系；Z-P-震旦系—二叠系；Pt-前震旦系；P2 β-峨眉山玄武岩；1.地质界线；2.向斜；3.背斜；4.实测推测正断层；5.实测推测逆断层
Fig.2. Structure outline map of the Daliangzi lead-zinc deposit
