内蒙古翁牛特旗西炮手营子铅锌矿床地质特征及找矿远景  

Geological features and prospecting prospect of Xipaoshouyingzi lead zinc deposit in Wengniute Banner,Inner Mongolia

作　　者：马冰心[1] 辛永辉 MA Bingxin;XIN Yonghui(Team 607,Bureau of Nonferrous Metals Geological Exploration of Jilin Province,Jilin 132013,Jilin,China)

机构地区：[1]吉林省有色金属地质勘查局六0七队,吉林吉林市132103

出　　处：《吉林地质》2024年第4期42-48,共7页Jilin Geology

摘　　要：研究区处于内蒙古大兴安岭弧盆系,温都尔庙-套苏沟俯冲增生杂岩带东部,并处于大兴安岭中南部多金属成矿带之河盛源-乌丹铀钼多金属成矿带中东部。矿体产出受构造控制,矿床成因类型为中温热液充填型脉状铅锌矿床。本区成矿地质条件优越,构造控矿特征明显。通过对矿床形成环境、成矿规律、找矿前景的研究分析,认为本区具有较好的找矿远景。The study area is situated within the arc-basin system of the Greater Khingan Mountains,Inner Mongolia.It is located in the eastern part of the Wenduermiao-Taosugou subduction accretion complex and in the central eastern part of the Heshengyuan-Wudan uranium-molybdenum polymetallic metallogenic belt of the central southern part of the Greater Khingan Mountains.The ore body output is controlled by structure,and the genetic type of deposit is a medium-temperature hydrothermal filling type vein lead-zinc deposit.The metallogenic geological conditions in this area are excellent,with obvious structural ore-controlling characteristics.Through studying and analyzing the forming environment,metallogenic regularity,and prospecting potential of the deposit,it is considered that this area has promising prospects for exploration.

关 键 词：内蒙古 矿体特征 铅锌 矿床 构造 找矿远景 

分 类 号：P618.4[天文地球—矿床学]