摘要
审章塘钨多金属矿矿床地质特征为矽卡岩型钨铅锌多金属矿床,矿床成因类型属接触交代矽卡岩型钨铅锌多金属矿床。本文拟以对审章塘钨多金属矿矿床成因与地层、构造、岩浆岩及围岩蚀变的关系进行研究,分析矿区找矿方向及找矿标记。
The geological characteristics of Shenzhangtang tungsten polymetallic deposit are skarn-type tungsten-leadzinc polymetallic deposit, and the genetic type of deposit is a metasomatic skarn type tungsten-lead-zinc polymetallic deposit.In this paper, the relationship between formation and strata, tectonics, magmatic rock and surrounding rock alteration and the prospecting direction and prospecting mark is studied.
出处
《世界有色金属》
2017年第17期93-94,共2页
World Nonferrous Metals
关键词
钨多金属矿
矿床成因
找矿方向
找矿标记
tungsten polymetallic
genetic type of deposit
prospecting direction
prospecting mark
