摘要
玉岭多金属矿为锡多金属矿床,矿床主要成因类型属岩浆气化-高中温热液充填交代矿床。结合生产资料及勘查成果,简述玉岭锡多金属矿矿床地质特征,并总结区内找矿标志。
The Yu Ling polymetallic ore is a tin polymetallic deposit. The main genetic type of the deposit belongs to the metasomatism of the magmatism - high - middle - high - temperature hydrothermal filling. Combining with the production data and exploration results, the geological characteristics of polymetallic ore deposit in the jade Lingxi, and summarizes the area prospecting marks.
作者
禹俊
YU Jun((The First Team of Hunan Nonferrous Geological Prospecting Bureau, Chenzhou 423000,Chin)
出处
《世界有色金属》
2018年第4期119-120,122,共3页
World Nonferrous Metals
关键词
锡多金属矿
矿床地质特征
找矿标志
tin polymetallic ore
geological characteristics of ore deposit
prospecting mark