河南黄金山重晶石矿床地质特征与矿床成因  

Geological Characteristics and Genesis of the Huangjinshan Barite Deposit in Henan Province

作　　者：郭钢阳 崔东豪 GUO Gang-yang;CUI Dong-hao(Henan Third Geological Exploration Institute Co.,Ltd.,Zhengzhou 450014,China;Henan Provincial CPC Party School,Zhengzhou 453002,China;Henan First Geology and Mineral Survey Institute Co.,Ltd.,Luoyang 471026,China)

机构地区：[1]河南省第三地质勘查院有限公司,河南郑州450014 [2]中共河南省委党校,河南郑州453002 [3]河南省第一地质矿产调查院有限公司,河南洛阳471026

出　　处：《中国非金属矿工业导刊》2024年第1期66-70,共5页China Non-Metallic Minerals industry

摘　　要：黄金山重晶石矿位于华北地台南缘,成矿地质条件优越。重晶石矿赋存于熊耳群马家河组安山岩,共圈出两个工业矿体。近矿围岩蚀变类型有硅化、绢云母化、绿泥石化、碳酸盐化等,其中硅化、碳酸盐化和绿泥石化与成矿关系密切;找矿标志有断裂构造标志及围岩蚀变标志;重晶石矿床受断裂构造、地层岩性和岩浆活动等因素联合控制,为热液充填型矿床。The Huangjinshan barite mine is located on the southern edge of the North China platform,with superior geological conditions for mineralization.The barite deposit occurs in the andesite of the Majiahe formation of the Xiong'er group,and two industrial ore bodies are circled.The types of wall rock alteration near the mine include silicification,sericitization,chloritization,carbonation,etc.Among them,silicification,carbonation,and chloritization are closely related to mineralization.The prospecting indicators include fault structure indicators and rock alteration indicators.The Huangjinshan barite deposit is controlled by factors such as fault structure,stratigraphic lithology,and magmatic activity,and is a hydrothermal filling type deposit.

关 键 词：渑池县 重晶石矿床 地质特征 控矿因素 

分 类 号：P619.251[天文地球—矿床学]