江西省上高县月光山铅锌矿地质特征与成因分析  

Geological characteristics and genetic analysis of the Yueguangshan lead-zinc deposit in Shanggao County,Jiangxi Province

作　　者：黄小海 HUANG Xiao-hai(Ecological Geology Brigade of Jiangxi Geological Bureau,Nanchang 330025,China)

机构地区：[1]江西省地质局生态地质大队,江西南昌330025

出　　处：《世界有色金属》2024年第21期37-39,共3页World Nonferrous Metals

摘　　要：月光山矿区铅锌矿床位于江南东部九岭隆起南部,萍乡—乐平坳陷带中东部,矿床区域上出露晚古生代石炭系上统马平组(C_(2)m)和二叠系下统栖霞组(P_(1)q)地层,断裂构造发育,岩浆活动强烈,成矿地质条件较好。综合区域地质背景、矿区、特征及矿体特征等,初步分析了月光山铅锌矿地质特征与成因分析。The lead zinc deposit in the Yueguangshan mining area is located in the southern part of the Jiuling Uplift in the eastern part of Jiangnan,in the central and eastern parts of the Pingxiang Leping Depression.The deposit area is exposed to the Late Paleozoic,Carboniferous Upper Maping Formation(C_(2)m)and Permian Lower Qixia Formation(P_(1)q)strata,with developed fault structures,strong magmatic activity,and good ore-forming geological conditions.Based on the comprehensive regional geological background,mining area,characteristics,and ore body characteristics,a preliminary analysis was conducted on the geological characteristics and genesis of the Yueguangshan lead-zinc deposit.

关 键 词：铅锌 矿体地质特征 成因分析 

分 类 号：P618[天文地球—矿床学]