摘要
门古-桥上一带位于扬子准地台北缘,为一中新元古代-古生代裂陷槽。上震旦统灯影组为含炭碎屑岩-碳酸盐岩建造,多期的构造-热液迭加作用,形成Pb、Zn矿化带沿青峰断裂带分布。基于该区铅锌矿成矿地质条件分析,推断该区有较佳的找矿前景。
The Mengu - Qiaoshang area on the northern margin of the Yangtze paraplatform is a Middle - Upper Proterozoic - Palaeozoic aulacogen, where occur clastic - carbonate formations of Upper Sinian Dengying Formation , in which developed lead - zinc mineralized belt along the Qingfeng fault belt. Based on the analysis of metal-logenic geological conditions, it is inferred that there will be a potential area to find lead - zinc deposits.
出处
《湖北地矿》
2004年第1期11-16,共6页
Hubei Geology & Mineral Resources
关键词
铅锌矿
矿床地质
成矿条件
找矿前景
Lead - zinc deposit Ore - forming conditions Exploration perspective Mengu - Qiaoshang
