赣县罗井坵钨多金属矿地质特征及成因探讨  

Geological characteristics and genesis of tungsten polymetallic ore deposit in Ganxian

作　　者：黄江洪[1] 曾祥骏 李灯平[1] 

机构地区：[1]江西有色地质勘查二队,江西赣州341000

出　　处：《世界有色金属》2017年第15期185-186,共2页World Nonferrous Metals

摘　　要：罗井坵钨多金属矿区有石英脉型、矽卡岩化型、蚀变花岗岩型含钨多金属矿(化)体以及破碎带型银矿体。通过前期地质找矿勘查,对矿区矿体的分布、形态、产状、规模、矿石质量与矿物共生有利一定了解,综合研究探讨成矿规律,为矿区找矿突破进行指导。The Luojingqi tungsten polymetallic deposit has quartz vein type, skarn type, altered granite type tungstencontaining polymetallic ore body and broken zone type silver ore body. Through the preliminary geological prospecting exploration, it is necessary to understand the distribution, shape, shape, scale, ore quality and mineral symbiosis of the ore body in the mining area, and comprehensively study the mineralization regularity to guide the prospecting breakthrough.

关 键 词：钨多金属 地质特征 成因探讨 

分 类 号：P597.3[天文地球—地球化学]