吉林省桦甸市大瓮泉沟金多金属矿地质特征浅析  

Geological characteristics of dawengquangou gold polymetallic deposit,Huadian City,Jilin Province

作　　者：赵晓阳[1] 胡平[1] 解馨竹 ZHAO Xiao-yang;HU Ping;XIE Xin-zhu(Team 604,Jilin Nonferrous Metals Geological Exploration Bureau,Jilin 132000,China)

机构地区：[1]吉林省有色金属地质勘查局六0四队

出　　处：《世界有色金属》2019年第19期282-282,284,共2页World Nonferrous Metals

摘　　要：勘查区位于桦甸市北东方向70km。通过近年来对该区域进行地质勘查工作,大致查明了工作区内成矿地质背景,物化探异常特征和矿化蚀变特征。获得多处土壤地球化学异常,物探激电中梯异常,利用槽探钻探工程控制一条矿化蚀变带,控制长约800m。带内见两条金矿化体,呈近东西向展布。The exploration area is 70km northeast of Huadian city.In recent years,through the geological exploration work in this area,the geological background of mineralization,the characteristics of geophysical and geochemical anomalies and the characteristics of mineralization and alteration in the work area have been roughly ascertained.Many geochemical anomalies of soil and ladder anomalies in IP are obtained.A mineralized alteration zone is controlled by trenching drilling engineering,with a length of about 800m.There are two gold mineralized bodies in the belt,which are distributed in nearly east-west direction.

关 键 词：大瓮泉沟金多金属矿 地质特征 吉林省桦甸市 

分 类 号：P618.2[天文地球—矿床学]