柴家沟钼多金属矿物化探特征与矿床成因分析  

Geochemical exploration characteristics and ore genesis analysis of Chaijiagou molybdenum polymetallic minerals

作　　者：马天意 MA Tian-yi(The Fourth Geological Brigade of Hebei Geological and Mineral Exploration and Development Bureau(Hebei Water Source Conservation Research Center),Chengde 067000,China)

机构地区：[1]河北省地质矿产勘查开发局第四地质大队(河北省水源涵养研究中心),河北承德067000

出　　处：《世界有色金属》2024年第13期106-108,共3页World Nonferrous Metals

摘　　要：为了能更好地开发我省平泉市柴家沟多金属矿产资源,本文在柴家沟钼矿以往勘查工作基础上,结合最新物化探工作成果,通过地物化工作和少量探矿工程等工作手段,大致查明矿区地质特征、蚀变矿化特征等,对柴家沟矿区矿体南部延伸情况进行控制,并从矿床地质特征、化探异常特征等对矿床成因进行分析探讨,从而使开采企业对柴家沟钼多金属矿产资源的开采更加安全高效。In order to better develop the polymetallic mineral resources in Chaijiagou,Pingquan City,our province,this article builds on the previous exploration work of Chaijiagou Molybdenum Mine and combines the latest results of physical and chemical exploration work.Through geological and chemical work and a small amount of exploration engineering,the geological characteristics,alteration and mineralization characteristics of the mining area are roughly identified.The southern extension of the ore body in Chaijiagou mining area is controlled,and the genesis of the deposit is analyzed and discussed from the geological characteristics and abnormal characteristics of chemical exploration,so as to make the mining of Chaijiagou molybdenum polymetallic mineral resources safer and more efficient for mining enterprises.

关 键 词：柴家沟 钼多金属矿 物化探 矿床成因 

分 类 号：P618.2[天文地球—矿床学]