浅析辽宁省辽阳县牛东沟金多金属矿成矿地质背景及控矿因素  

Analysis on the Geological Setting of Ore-forming Processes and Ore-controlling factors of Niudonggou Gold Polymetallic Deposit in Liaoyang County,Liaoning Province

作　　者：李飞 蒋永臻 李乃琨 LI Fei;JIANG Yong-zhen;LI Nai-kun(Liaoning Non-ferrous Geological Exploration and Research Institute Co.,Ltd.,Shenyang 110013,China)

机构地区：[1]辽宁有色勘察研究院有限责任公司,辽宁沈阳110013

出　　处：《有色矿冶》2025年第1期6-11,共6页Non-Ferrous Mining and Metallurgy

基　　金：辽宁省级地质勘查项目:编号:LNZC2019-0076-20(1)。

摘　　要：牛东沟金多金属矿位于辽宁省辽阳县隆昌镇林场-八会镇龙凤峪,矿区位于塔子岭-五龙金多金属矿成矿带的北端,区内发现7条含矿石英脉,编号1~7号,其中:金银矿化2条,金矿化1条,铅锌矿化4条;形成矿体2条。含矿石英脉多呈北北东、近南北向展布,受北东向张性断裂构造控制,石英脉多平行脉产出。The Niudonggou gold-polymetallic mine is situated in the northern end of the Taziling-Wulong gold-polymetallic mine prospecting Trend,located in Linchang of Longchang Town~Longfengyu of Bahui town,Liaoyang County,Liaoning Province.Seven mineralized quartz veins have been identified in this area,numbered 1 to 7,among them,there are two gold and silver mineralization zones,one gold mineralization zone,and four lead and zinc mineralization zones;.Two ore bodies have formed.Ore-bearing veins are mostly distributed in north-northeast and near south-north,controlled by the northeastward tensile fault structure,the quartz veins are produced in parallel.

关 键 词：牛东沟 金多金属矿 成矿地质背景 控矿因素 

分 类 号：P618.51[天文地球—矿床学]