摘要
审章塘钨多金属矿床属典型矽卡岩型白钨矿床,矿床成矿规律为接触交代矽卡岩型钨铅锌多金属矿床。对审章塘矿区钨多金属矿矿床成矿地质背景、矿床地质特征、矿床成矿规律进行分析。
Shenzhangtang tungsten polymetallic deposit is a typical skarn type scheelite deposit,and its metallogenic regularity is contact metasomatic skarn type tungsten lead zinc polymetallic deposit.This paper analyzes the metallogenic geological background,geological characteristics and metallogenic regularity of the shenzhangtang tungsten polymetallic deposit.
作者
罗四华
LUO Si-hua(First Team of Hunan Nonferrous Metals Geological Exploration Bureau,Chenzhou 423000,China)
出处
《世界有色金属》
2021年第10期180-182,185,共4页
World Nonferrous Metals
关键词
钨多金属矿
矽卡岩型矿床
地质特征
成矿规律
湖南省道县
审章塘
tungsten polymetallic ore
Skarn type deposit
Geological characteristics
Metallogenic regularity
Daoxian County,Hunan Province
Shen Zhang Tang