湖南重晶石矿基本地质特征
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摘要
湖南省衡南县地处衡阳盆地中部地带。县境西北及东部环山,中部丘陵起伏,地势从东、南、西三面向北逐渐倾斜,构成凹字形丘陵盆地并向北开口。文章通过对衡南县重晶石矿产资源的工业类型、地质特征、矿区组合、物理特性等基础数据进行统计分析,对于湖南省衡南县重晶石矿资源保障程度、资源富集度、开发利用率、开发潜力等方面具有推进作用,也存在较好的找矿远景。
Hengnan County, Hunan Province is located in the central region of the Hengyang basin. The northwest mountains in the East and central hilly terrain from East, South, West three north facing gradually tilted to form a concave shape and open in the North hilly basin. This paper makes the statistical analysis of the basic data of Hengnan County barite mineral resources industrial type, geologic characteristics, composition, physical properties, Hengnan County of Hunan Province that the barite ore has a large scale, high degree of resource security and resource rich degree is concentrated, development and utilization rate is higher, the advantage of great development potential.
Hengnan County, Hunan Province is located in the central region of the Hengyang basin. The northwest mountains in the East and central hilly terrain from East, South, West three north facing gradually tilted to form a concave shape and open in the North hilly basin. This paper makes the statistical analysis of the basic data of Hengnan County barite mineral resources industrial type, geologic characteristics, composition, physical properties, Hengnan County of Hunan Province that the barite ore has a large scale, high degree of resource security and resource rich degree is concentrated, development and utilization rate is higher, the advantage of great development potential.
引文
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[3]韩善楚,胡凯,曹剑.贵州天柱早寒武世黑色岩系重晶石矿床有机地球化学研究[J].地球化学,2014,43(4):386-398.
[4]刘波.四川省绵竹市英雄崖重晶石矿床地质特征及开采技术条件研究[J].四川有色金属,2016.39-42.
[5]陈先沛.层控重晶石矿床地球化学.见:涂光炽主编.中国层控矿床地球化学(第二卷)[M].北京:科学出版社,1987.163-171.
[6]Michard A,et al.Rare earth elements and uranium in high-temperature solutions from East Pacific Rise hydrothermal vent field(13N)[J].Nature,1983,303:795~797.
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[8]Fleet A J.Hydrothermal and hydrogeneous ferromanganes deposits.In:Rona P A,et al,eds.HydrothermalProcesses at Seafloor Spreading Centers.New York:Plenum Press,1983.537-570.