摘要
通过总结会东长新铅锌矿地质特征,分析了控矿因素,对矿体的成因进行了探讨;矿化富集层位位于下寒武系组白云岩,距下寒武系麦地坪组顶部0~10m的白云岩中,属沉积改造型矿体;指出了找矿方向及建议,为今后该地区铅锌找矿工作提供了参考。
By summarize geological characteristics of the Changxin Pb-Zn deposit, analyzed the mine-controlling factors, discussed the causes of mine. The mineralization layer is located in the under Cambrian dolomite which from the top of Maidiping group to 10 meters, belongs to sedimentary mine. It points out the prospecting direction and recommendations, provide a reference for future work in the area.
出处
《世界有色金属》
2016年第15期103-104,共2页
World Nonferrous Metals
关键词
铅锌矿
地质特征
找矿方向
会东长新
Pd-Zn deposit
geological features
prospecting direction
Changxin
