摘要
下志留统湾塘组地层是Zn、Pb含矿层位。NW向、NE向低序次破碎带的转折处,不同能干性岩层接触部位为层状、似层状锌矿体产出的重要场所;NNE向次级构造控制陡倾斜脉状矿体。
The Lower Silurian Wantang Formation is the Pb -Zn -bearing ore bed. The important places of stratiform, stratoid Pb - Zn orebody occurrence are the turning part of NW, NE subordinate fractured zone and interstratal fractured zone and the contact part of different rock beds. The steep veined orebody is controlled by the NNE subordinate structure.
出处
《云南地质》
2007年第1期41-48,共8页
Yunnan Geology
关键词
锌致矿异常
破碎带控矿
下志留统湾塘组
金平云南
Metallogenetic Anomaly of Zn
Lower Silurian Wantang Formation
Ore - Controlling Fractured Zone
Jinping, Yunnan
