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

作　　者：周润民 柯帅 ZHOU Run-min;KE Shuai(Baoji Northwest Nonferrous Erlihe Mining Co.,Ltd,Baoji 721000,China Abstract:The peripheral lead-zinc copper deposit of Yinmu Temple is located in the secondary)

机构地区：[1]宝鸡西北有色二里河矿业有限公司,陕西宝鸡721000

出　　处：《世界有色金属》2024年第4期121-123,共3页World Nonferrous Metals

摘　　要：银母寺外围铅锌铜矿位于凤太金铅锌矿集区西部的次级热水沉积盆地中,成矿条件优越,已探明银母寺中型铅锌矿床及多个小型铅锌矿床。文中主要针对银母寺外围铅锌铜矿地质特征进行详细分析,并探讨该矿矿床成因,希望通过本文研究,能对该区找矿工作提供一些参考作用。The peripheral lead-zinc copper deposit of Y inmu T emple 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 Y inmu T emple 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 Y inmu T emple,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 

分 类 号：P618.4[天文地球—矿床学]