世界有色金属Issue(4)：121-123,3.
陕西省凤县银母寺外围铅锌铜矿地质特征及成因研究
Geological characteristics and genesis of lead zinc copper deposits in the peripheral area of Yinmu Temple,Feng County,Shaanxi Province
周润民 1柯帅1
作者信息
- 1. 宝鸡西北有色二里河矿业有限公司,陕西 宝鸡 721000
- 折叠
摘要
Abstract
The peripheral lead-zinc copper deposit of Yinmu Temple is located in the secondary hot water sedimentary basin in the western part of the Fengtai gold lead-zinc deposit concentration area,with superior ore-forming conditions.It has been discovered that Yinmu Temple has a medium-sized lead-zinc deposit and multiple small-scale lead-zinc deposits.The article mainly conducts a detailed analysis of the geological characteristics of the lead zinc copper deposit in the peripheral area of Yinmu Temple,and explores the genesis of the deposit.It is hoped that this study can provide some reference for the exploration work in the area.关键词
银母寺外围铅锌铜矿/地质特征/矿床成因/陕西省凤县Key words
lead zinc copper mine around Yinmu Temple/Geological characteristics/Origin of mineral deposits/Feng County,Shaanxi Province分类
天文与地球科学引用本文复制引用
周润民,柯帅..陕西省凤县银母寺外围铅锌铜矿地质特征及成因研究[J].世界有色金属,2024,(4):121-123,3.
