摘要
棋盘石铅锌多金属矿属于矽卡岩型多金属矿。通过对该矿床地质特征的分析后认为,矿体严格受岩体、碳酸盐岩及构造的控制,矿石类型为矽卡岩型硫化铅锌矿石;围岩蚀变以黄铁矿化、矽卡岩化、绿泥石化、碳酸盐化为特征;岩体与碳酸盐岩接触带为该矿床的重要的找矿方向。
The Qipanshi lead-zinc polymetallic deposit belongs to skarn type polymetallic deposit. lhrougla the analysis on the geological characteristics of the deposit, there are 3 conclusions can be reached： 1） orebody is strictly controlled by the rock, carbonate rock and structure,ore types for the skarn Pb Zn sulphide ore; 2）wall rock alterationpyritization, skarn, chloritization, carbonatation; 3）rock andcarbonate rock in contact with the deposit the important ore prospecting marks.
出处
《化工矿产地质》
CAS
2013年第4期234-241,共8页
Geology of Chemical Minerals
关键词
铅锌多金属矿
地质特征
找矿地质前提
找矿标志
腾冲县
棋盘石
lead-zinc polymetallic deposit, geological characteristics, geological preconditions for prospecting, prospecting cariteria, Tengchongcounty, Qipanshi
