青阳县来龙山方解石矿第九第十矿段地质特征及控矿因素  

Geological Characteristics and Ore-controlling Factors of Lailongshan Calcite Mine Ninth and Tenth Block in Qingyang County

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作  者:刘川云 LIU Chuanyun(No.321 Geological team,Bureau of Geology and Mineral Exploration of Anhui Province)

机构地区:[1]安徽省地质矿产勘查局321地质队

出  处:《现代矿业》2023年第5期9-13,共5页Modern Mining

摘  要:为指导方解石找矿工作,在结合相关地质成果基础上,对安徽省青阳县来龙山方解石矿第九第十矿段的区域地质背景、矿床地质特征进行分析,研究了地层、构造、岩浆岩等控矿因素对方解石成矿的影响。结果表明,矿床具有接触变质型方解石矿床的一般地质特征,可在与该矿区的地层、构造情况类似的区域开展勘查工作。In order to guide the calcite prospecting work,based on the related geological and explora⁃tion results,the regional geological background and geological characteristics of the deposit in the 9th and 10th block of Lailongshan Calcite Mine in Qingyang County,Anhui Province were analyzed,and the influ⁃ence of ore-controlling factors such as strata,structure and magmatic rock on the calcite mineralization was studied.The results show that the deposit has the general geological characteristics of contact metamorphic calcite deposit.The exploration work can be carried out in areas similar to the mining area,strata and struc⁃ture.

关 键 词:方解石矿 区域地质背景 地质特征 控矿因素 

分 类 号:P619.2[天文地球—矿床学]

 

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