广东省英德市杉木塘铅锌多金属矿矿床成因及找矿标志  

Genesis and Prospecting Indicators of the Shanmutang Lead-zinc Polymetallic Deposit in Yingde City,Guangdong Province

作　　者：龙勇 Long Yong(Team 940,Guangdong Nonferrous Metals Geological Bureau,Qingyuan Guangdong 511500,China)

机构地区：[1]广东省有色金属地质局九四〇队,广东清远511500

出　　处：《山西冶金》2024年第10期95-97,共3页Shanxi Metallurgy

摘　　要：杉木塘铅锌矿位于粤北曲江—英德断陷盆地,地处南岭纬向构造带的中段。出露地层主要有古生代下石炭统石磴子组(C1s)及新生界第四系(Q)等,矿床成因类型属中低温热(汽)液构造活动成矿。主要对区域地质背景、矿区地质特征、围岩蚀变及矿体特征等进行分析,并研究了该区矿床成因及找矿标志,为下一步找矿指明了方向。The Shanmutang Pb Zn deposit is located in the Qujiang Yingde fault basin in northern Guangdong,in the middle of the the Nanling Mountain latitudinal structural belt.The exposed strata mainly include the Lower Carboniferous Shidengzi Formation(C1s)of the Paleozoic era and the Quaternary System(Q)of the Cenozoic era.The genesis type of the deposit belongs to the medium low temperature hydrothermal tectonic activity mineralization.It mainly analyzed the regional geological background,mining area geological characteristics,surrounding rock alteration,and ore body characteristics,studied the genesis and prospecting indicators of the ore deposit in the area,and pointed out the direction for the next step of prospecting.

关 键 词：杉木塘铅锌矿 矿床成因 找矿标志 

分 类 号：TD862[矿业工程—金属矿开采]