探究随县王家台金银钨多金属矿地质特征及矿床成因
Exploring the geological characteristics and genesis of the Wangjiatai gold silver tungsten polymetallic deposit in Suixian County
许涛 1吴松 1牛志勇 1曾琳 1刘杰1
作者信息
- 1. 湖北省地质局第八地质大队,湖北 襄阳 441000
- 折叠
摘要
王家台金银钨多金属矿是湖北随县发现的一重要的金银钨多金属矿,该矿位于湖北省随县的北部,大地构造为扬子板块和华北板块的随应高压浅变质地体北缘,成矿区为东秦岭Au-Ag-Mo-Cu-Pb-Zn-Sb金属成矿带之随枣地区金银成矿亚带.区内断裂构造发育,成矿地质条件优越,成矿潜力巨大.为了寻求更大的找矿突破,本文中主要对该矿地质特征进行分析探讨,并研究其矿床成因,希望能为该矿找矿工作提供一些借鉴与参考.
Abstract
The Wangjiatai gold silver tungsten polymetallic deposit is an important gold silver tungsten polymetallic deposit discovered in Suixian County,Hubei Province.The deposit is located in the northern part of Suixian County,Hubei Province.The geological structure is the northern edge of the corresponding high-pressure shallow metamorphic terrane of the Yangtze and North China plates,and the mineralization area is the Suizao gold silver mineralization sub zone of the East Qinling Au Ag Mo Cu Pb Zn Sb metal mineralization belt.The area has developed fault structures,superior geological conditions for mineralization,and huge potential for mineralization.In order to seek greater breakthroughs in ore exploration,this article mainly analyzes and explores the geological characteristics of the mine,and studies the genesis of its deposit,hoping to provide some reference and reference for the ore exploration work of the mine.
关键词
王家台金银钨多金属矿/地质特征/矿床成因/湖北随县Key words
Wangjiatai gold silver tungsten polymetallic ore/Geological characteristics/Genesis of mineral deposits/Suixian County,Hubei Province引用本文复制引用
出版年
2024
国家科技期刊平台
NSTL
万方数据