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安徽含山地区横山萤石矿地质特征及找矿前景分析

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安徽省含山县横山萤石矿位于巢湖—含山复背斜的轴部,区内断层发育,地层以奥陶系碳酸岩为主.根据探矿工程揭露,矿体主要赋存奥陶系的灰岩、和泥质灰岩及少量白云岩和白云质灰岩中的构造裂隙中.矿体形态受断层破碎带控制,矿体走向北东,倾向北西向,CaF2平均品位为53.57%,矿区围岩主要发生硅化,次为大理岩化、重晶石化,局部铁锰矿化等,矿床成因类型为中—低温热液型交代矿床.通过总结矿体地质特征及矿床成因,证实横山背斜断层破碎带发育位置存在较好的找矿前景,同时矿体深部及外围均未充分控制,本区仍具有较好的找矿前景.
Geological Characteristics and Prospecting Prospects Analysis of Hengshan Fluorite Deposit in the Hanshan Area of Anhui Province
The Hengshan fluorite mine in Hanshan County,Anhui Province is located on the axis of the Chaohu Hanshan anticline,with well-developed faults and mainly composed of Ordovician carbonate rocks.According to the exploration project,the ore body mainly exists in the structural fractures of Ordovician limestone,mudstone limestone,and a small amount of dolomite and dolomitic limestone.The shape of the ore body is controlled by the fault fracture zone,with a strike northeast and dip northwest.The average CaF2 grade is 53.57%.The surrounding rock of the mining area mainly undergoes silicification,followed by marbling,baritization,and local iron manganese mineralization.The genesis type of the deposit is a medium to low temperature hydrothermal metasomatic deposit.By summarizing the geological characteristics and genesis of the ore body,it is confirmed that there is a good prospecting prospect for the development of the Hengshan anticline fault fracture zone.At the same time,the deep and peripheral parts of the ore body are not fully controlled,and this area still has good prospecting prospects.

geological featuresexploration prospectsHengshan fluorite mineAnhui Hanshan Region

刘为好、陆中秋

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安徽省地质矿产勘查局322地质队,安徽 马鞍山 243000

地质特征 找矿前景 横山萤石矿 安徽含山地区

2024

山西冶金
山西省金属学会 山西省有色金属学会

山西冶金

影响因子:0.139
ISSN:1672-1152
年,卷(期):2024.47(1)
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