摘要
滴水坎箐铅矿矿体赋存于中侏罗统花开左组下段含砾石英砂岩、长石石英砂岩中,圈出矿体2条,矿体具有典型的层控特征。同时,北北东向构造对矿体形成亦有控制作用。
The drop water canqing lead ore deposit occurs in the Middle Jurassic in the left lower section of the gravel quartz sandstone and feldspar quartz sandstone,and 2 ore bodies are trapped,and the orebodies have typical layer control characteristics.At the same time,the NNE structure also controls the formation of ore bodies.
作者
洪建磊
程云茂
黄金龙
李刚
赵艳林
HONG Jian-lei;CHENG Yun-mao;HUANG Jin-long;LI Gang;ZHAO Yan-lin(Southwest nonferrous metals Kunming survey and Design Institute(Limited by Share Ltd),Kunming 650093,China)
出处
《世界有色金属》
2018年第9期184-185,187,共3页
World Nonferrous Metals
关键词
矿源层
构造影响
成矿地质条件
滴水坎箐铅矿
云南澜沧
ore source bed
structural influence
metallogenic geological condition
dripping Kan Qing lead ore
Lancang,Yunnan