摘要
江城县松山林铅锌矿矿体呈似层状、透镜状产于近东西向的断层破碎带中,矿体近矿围岩为下白垩统景星组(K_1j),矿石岩性为碎裂岩化的石英砂岩、粉砂岩、岩屑石英砂岩;构造控矿明显,该铅锌矿为热液型矿床。沿断裂带分布的地球化学异常是重要的找矿标志。
The orebody of Songshanlin in Jiangcheng is stratoid,lenticular in nearly EW fault fracture zone.The wall rock near orebody is Lower Cretaceous Jingxing Formation（ K1 j）. The ore-bearing rock is fractured quartz sandstone,siltstone,lithic quartz sandstone. The ore control of structure is clear. It is a hydrothermal Pb-Zn deposit. The geochemical anomaly along the fault zone is the important prospecting criteria.
作者
杨丽梅
YANG Li-mei(Yunnan Institute of Geological Survey,Kunming 650217)
出处
《云南地质》
2018年第2期175-178,共4页
Yunnan Geology
关键词
构造控矿
热液型矿床
云南江城松山林
Ore Control of Structure
Hydrothermal Deposit
Songshanlin
Jiangeheng
Yunnan
