摘要
铅锌矿赋存于灯影组硅质条带白云岩中,局部产于筇竹寺组,脉状、透镜状,与峨眉山玄武岩喷发关系密切,属岩浆晚期热液成因。
The Pb-Zn deposit is in the Dengying Formation banded dolomitite,locally in the Qiongzhusi Formation,veined,lenticular.It is in close relation with the Emeishan basalt eruption and belongs to late magmatic hydrothermal genesis.
引文
[1]韩润生,陈进,黄智龙,马德云,薛传东,李元等,构造成矿动力学及隐伏矿定位预测-以云南会泽超大型铅锌(银、锗)矿床为例[M].北京:科学出版社.2006.
[2]姚凤良、孙丰月,矿床学教程[M].北京:地质出版社.2005.
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