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物探与化探  2024, Vol. 48 Issue (1): 15-23    DOI: 10.11720/wtyht.2024.2588
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
河南省方城县莫沟萤石矿床地质特征及成因
张青松1,2(), 夏明哲1(), 王春连3, 栗克坤2, 刘增政2, 蒋济勇2, 江建浪2
1.长安大学 地球科学与资源学院,陕西 西安 710054
2.中化地质矿山总局 河南地质局,河南 郑州 450000
3.中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室,北京 100037
Geological characteristics and origin of the Mogou fluorite deposit in Fangcheng County, Henan Province
ZHANG Qing-Song1,2(), XIA Ming-Zhe1(), WANG Chun-Lian3, LI Ke-Kun2, LIU Zeng-Zheng2, JIANG Ji-Yong2, JIANG Jian-Lang2
1. School of Earth Science and Recourses, Chang'an University, Xi'an 710054, China
2. Henan Geological Bureau of CCGMB, Zhengzhou 450000, China
3. MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
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摘要 

方城县莫沟萤石矿床是河南省南部萤石成矿带的主要组成部分之一,产于新元古界煤窑沟组内。本文在剖析莫沟萤石矿床地质特征的基础上,开展了岩相学、岩石地球化学研究,约束了成矿物质来源,探讨了矿床成因机制。结果表明:萤石矿体呈脉状、透镜状产出,与成矿有关的蚀变有硅化、萤石化、绢云母化等,矿石构造类型主要为块状,次为条带状、条纹状、角砾状。萤石矿体与煤窑沟组大理岩、燕山期似斑状斜长花岗岩的球粒陨石标准化稀土元素配分模式基本一致,显示成矿物质来源与煤窑沟组大理岩和燕山期似斑状斜长花岗岩有关,应为富含F元素的含矿热液沿层间断层侵入并与围岩发生反应,沉淀形成萤石矿(化)体,矿床成因类型为低温热液沿层间构造充填型矿床。
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张青松
夏明哲
王春连
栗克坤
刘增政
蒋济勇
江建浪
关键词 ： 萤石矿床,  矿床特征,  稀土元素,  成矿物质,  成因,  成矿模式    
Abstract：

The Mogou fluorite deposit of Fangcheng County, residing in the Neoproterozoic Meiyaogou Formation, is a crucial part of the fluorite metallogenic belt in southern Henan Province. Based on the analysis of the geological characteristics of the Mogou fluorite deposit, this study conducted petrographic and petrogeochemical studies to define the source of ore-forming materials and probe into the genetic mechanism of the fluorite deposit. The results show that the fluorite ore body is veined or lenticular, with mineralization-related alterations composed of silicification, fluorite and sericite alterations. Its ore structures are primarily massive, followed by banded, striped, and brecciated types. The chondrite-normalized rare earth element distribution pattern of the fluorite ore body is similar to that of the Meiyaogou Formation marbles and the Yanshanian porphyritic plagiogranites, suggesting a genetic relationship. The possible genetic mechanism is that the F-enriched ore-bearing hydrothermal liquids intruded along the interbedded fault and reacted with the surrounding rocks to form the fluorite ore /mineralized body. The deposit belongs to the epithermal filling type along the interbedded structure.
Key words： fluorite deposit    deposit characteristics    rare earth element    ore-forming materials    origin    metallogenetic mode
收稿日期: 2022-11-27      修回日期: 2023-06-26      出版日期: 2024-02-20
ZTFLH:  P632  
基金资助:中央级公益性科研院所基本科研业务费专项(KK2005);中国地质调查局地质矿产调查评价专项项目(DD20190816);中国地质调查局地质矿产调查评价专项项目(DD20190606)
通讯作者: 夏明哲(1979-),男,副教授,主要从事岩浆岩与岩浆矿床研究工作。Email:zymzxia@chd.edu.cn
作者简介: 张青松(1982-),男,高级工程师,主要从事地质矿产勘查研究工作。Email:153671157@qq.com
引用本文:   
张青松, 夏明哲, 王春连, 栗克坤, 刘增政, 蒋济勇, 江建浪. 河南省方城县莫沟萤石矿床地质特征及成因[J]. 物探与化探, 2024, 48(1): 15-23.
ZHANG Qing-Song, XIA Ming-Zhe, WANG Chun-Lian, LI Ke-Kun, LIU Zeng-Zheng, JIANG Ji-Yong, JIANG Jian-Lang. Geological characteristics and origin of the Mogou fluorite deposit in Fangcheng County, Henan Province. Geophysical and Geochemical Exploration, 2024, 48(1): 15-23.
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https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2024.2588      或      https://www.wutanyuhuatan.com/CN/Y2024/V48/I1/15
Fig.1  河南省方城县莫沟一带地质(a)及区域构造(b)
Fig.2  莫沟萤石矿区2勘探线地质剖面
Fig.3  方城县莫沟一带萤石矿及显微特征
a—沿裂隙充填萤石矿;b—块状萤石矿;c—紫色萤石与围岩变形特征;d—白色条带状萤石及沿裂隙发育的辉钼矿;e—钻孔内的条带状萤石;f—条带状萤石,单偏光;g—条带状萤石变形,正交偏光;Fl—萤石;Mot—辉钼矿;Ms—白云母;Cal—方解石;Phl—金云母;Qz—石英
Hf Ta W Pb Bi Th U Li Be
XT1 0.06 0.07 0.14 1.65 0.01 0.13 0.1 3.11 0.22
XT2 8.5 2.45 2.07 16.98 0.08 21.04 4.81 85.12 6.06
XT3 0.16 0.09 0.3 2.04 0.03 0.34 1.15 7.83 0.5
XT4 0.09 0.1 32.59 91.33 1.45 0.34 0.28 37.88 1.04
V Cr Co Ni Cu Zn Ga Rb Sr
XT1 2.09 2.1 2.93 10.29 2.65 2.46 0.89 1.55 242.78
XT2 148.98 138.61 20.5 41.09 25.43 127.36 27.09 212.67 213.94
XT3 2.29 3.34 3.19 10.4 3.12 3.76 1.31 3.67 82.8
XT4 5.43 2.91 2.97 10.17 8.47 51.4 1.63 8.68 63.68
Zr Nb Mo Cd In Sn Sb Cs Ba
XT1 2.16 0.19 0.08 0.01 0 0.12 6.87 0.13 11.03
XT2 297.37 33.65 7.89 0.37 0.13 4.73 3.68 19.35 820.13
XT3 5.57 0.79 0.19 0.02 0.01 0.17 6.86 0.42 18.05
XT4 2.31 0.5 5.23 0.66 0.01 0.23 6.7 1.69 11.3
Table 1  方城县莫沟萤石矿微量元素分析结果
Fig.4  方城县莫沟萤石矿微量元素蛛网(标准化数据据Sun等 [17])
岩矿石名称 萤石 萤石 萤石 萤石 萤石 萤石 萤石 大理岩 片岩 片岩
编号 XT1 XT2 XT3 XT4 XT5 XT6 XT7 XT8 XT9 XT10
La 5.87 64.08 11.85 9.24 8.45 7.4 6.52 3.85 10.8 18.41
Ce 10.20 135.69 21.48 18.03 16.6 14.9 13.7 7.31 17.9 37.91
Pr 1.12 15.34 2.15 2.24 2.11 1.78 1.7 0.79 3.33 4.57
Nd 3.87 58.51 6.91 8.93 7.89 6.86 6.62 2.96 15.4 18.07
Sm 1.20 11.61 1.53 2.61 1.9 1.57 1.57 0.66 4.15 3.90
Eu 0.42 2.65 0.41 0.96 0.54 0.4 0.42 0.23 1.58 1.17
Gd 1.58 11.51 2.05 3.71 2.2 1.86 1.88 0.81 4.37 4.56
Tb 0.29 1.53 0.38 0.68 0.4 0.31 0.34 0.13 0.68 0.61
Dy 1.92 8.31 2.72 4.62 2.09 1.8 1.77 0.72 3.7 3.51
Ho 0.41 1.53 0.64 0.98 0.46 0.36 0.37 0.15 0.7 0.67
Er 1.30 4.39 2.28 2.84 1.3 1.03 0.97 0.45 1.99 1.96
Tm 0.18 0.55 0.36 0.37 0.22 0.13 0.15 0.065 0.26 0.27
Yb 1.43 3.59 2.70 2.72 1.11 0.69 0.69 0.38 1.58 1.80
Lu 0.23 0.52 0.42 0.38 0.2 0.1 0.13 0.058 0.24 0.26
Y 24.67 40.40 46.65 53.54 17.1 16 15.1 5.23 17 18.95
ΣREE 30.02 319.81 55.90 58.29 45.47 39.19 36.83 18.56 66.68 97.68
LREE 22.68 287.89 44.33 42.01 37.49 32.91 30.53 15.80 53.16 84.03
HREE 7.35 31.92 11.57 16.28 7.98 6.28 6.30 2.76 13.52 13.65
w(LREE)/w(HREE) 3.09 9.02 3.83 2.58 4.70 5.24 4.85 5.72 3.93 6.16
[w(La)/w(Yb)]N 2.94 12.82 3.15 2.44 5.46 7.69 6.78 7.27 4.90 7.32
δEu 0.93 0.69 0.70 0.94 0.81 0.71 0.75 0.96 1.13 0.84
δCe 0.91 1.03 0.97 0.94 0.94 0.97 0.99 0.97 0.73 0.98
Table 2  方城县莫沟萤石矿稀土元素分析结果及特征值
Fig.5  方城县莫沟萤石矿稀土元素蛛网(标准化数据据Sun等[17],XT11为燕山期似斑状斜长花岗岩,数据自河南地质矿产厅[21])
Fig.6  方城县莫沟萤石矿[w(La)+w(Y)]-w(Y)/w(La)关系
Fig.7  方城县莫沟萤石矿w(Y)/w(Ho)-w(La)/w(Ho)关系
Fig.8  方城县莫沟一带萤石矿床成矿模式
[1] 陈军元, 刘艳飞, 颜玲亚, 等. 石墨、萤石等战略非金属矿产发展趋势研究[J]. 地球学报, 2021, 42(2):287-296
[1] Chen J Y, Liu Y F, Yan L Y, et al. News sciencemagorgsciencenow Study on the development trend of graphite,fluorite and other strategic nonmetallic minerals[J]. Journal of the Earth, 2021, 42(2):287-296.
[2] 王宏海. 将乐萤石矿床地质特征及成因[J]. 地质与勘探, 1991(3):21-43.
[2] Wang H H. Geological feature and genesis of Jiangle fluorite deposit[J]. Geology and Prospecting, 1991(3):21-43.
[3] 王吉平, 商朋强, 熊先孝, 等. 中国萤石矿床分类[J]. 中国地质, 2014, 41(2):315-325.
[3] Wang J P, Shang P Q, Xiong X X, et al. Classification of fluorite deposits in China[J]. Geology in China, 2014, 41(2):315-325.
[4] 吴自强, 谢从智. 中国萤石矿床地质与勘探[M]. 北京: 地质出版社, 1989:28-40.
[4] Wu Z Q, Xie C Z. China Fluorspar Deposit Geology and Exploration[M]. Beijing: Geological Publishing House, 1989:28-40.
[5] 陈新立, 刘增政, 栗克坤. 闽北地区萤石矿赋矿硅化带地质及地球化学特征.[J]. 化工矿产地质, 2018, 40(3):155-161.
[5] Chen X L, Liu Z Z, Li K K. Geologocal and geochenmical characteristics of Ore-bearing silicification zone for fluorite deposits in northern Fujian[J]. Geology of Chemical Minerals, 2018, 40(3):155-161.
[6] 李士勤. 火山作用形成的特大型沉积萤石矿床[J]. 地质与勘探, 1985, 21(1):30-31.
[6] Li S Q. Gigascope sedimentary fluorite deposit formed by volcanism[J]. Geology and Prospecting, 1985, 21(1):30-31.
[7] 王吉平, 商朋强, 熊先孝, 等. 中国萤石矿床成矿规律[J]. 中国地质, 2015, 42(1):18-32.
[7] Wang J P, Shang P Q, Xiong X X, et al. Metallogenic regularities of fluorite deposits in China[J]. Geology in China, 2015, 42(1):18-32.
[8] 温同想. 方城萤石矿带地质特征[J]. 河南地质, 1997, 15(2):103-107.
[8] Wen T X. The geological characteristics of fluorite ore belt in FangCheng[J]. Henan Geology, 1997, 15(2):103-107.
[9] 张苏坤, 王辉, 冯绍平, 等. 河南省栾川县杨山萤石矿成矿作用:来自氢氧同位素和元素地球化学的约束[J]. 西北地质, 2022, 55(2):209-216.
[9] Zhang S K, Wang H, Feng S P, et al. Mineralization of Yangshan fluorite deposit in Luanchuan County,Henan Province:Constraints from H-O isotopes and element geochemistry[J]. Northwestern Geology, 2022, 55(2):209-216.
[10] 刘纪峰, 白德胜, 张凯涛, 等. 河南方城刘营萤石矿稀土元素特征及成矿年龄[J]. 物探与化探, 2021, 45(3):639-644.
[10] Liu J F, Bai D S, Zhang K T, et al. REE characteristics and metallogenic age of the Liuying fluorite deposit in Fangcheng,Henan Province[J]. Geophysical and Geochemical Exploration, 2021, 45(3):639-644.
[11] 刘振超, 李蒙, 聂艳敏, 等. 河南方城大张庄萤石矿地质特征及找矿标志[J]. 长春工程学院学报:自然科学版, 2019, 20(1):65-68,97.
[11] Liu Z C, Li M, Nie Y M, et al. The geological characteristics and prospecting indicatorsof the Dazhangzhuang fluorite deposit in Fangcheng,Henan Province[J]. Journal of Changchun Institute of Technology:Natural Sciences Edition, 2019, 20(1):65-68,97.
[12] 田培学. 南召—方城沉积变质型萤石矿床的若干特征[J]. 河南地质, 1984(1):9-15.
[12] Tian P X. Some characteristics of Nanzhao-Fangcheng sedimentary metamorphic fluorite deposit[J]. Henan Geology, 1984(1):9-15.
[13] 段世轻, 刘志如, 谢朝永. 嵩县杨山—车村—方城县一带萤石矿成矿地质特征研究[J]. 现代矿业, 2021, 3(3):19-22.
[13] Duan S Q, Liu Z R, Xie C Y. Study on the metallogenic geological characteristics of fluorite mine in Yangshan-Checun of Songxian County-Fangcheng County area[J]. Modern Mining, 2021, 3(3):19-22.
[14] 杨永印, 罗志阳, 郜松杰. 河南省方城县土门萤石矿控矿因素分析[J]. 西部探矿工程, 2012, 24(3):151-154.
[14] Yang Y Y, Luo Z Y, Gao S J. Analysis of ore control factors of Tumen fluorite mine in Fangcheng County,Henan Province[J]. Western Exploration Project, 2012, 24(3):151-154.
[15] 潘桂棠, 肖庆辉, 陆松年, 等. 中国大地构造单元划分[J]. 中国地质, 2009, 36(1):5-28.
[15] Pan G T, Xiao Q H, Lu S N, et al. Division of tectonic units in China[J]. Geology in China, 2009, 36(1):5-28.
[16] 徐志刚, 陈毓川, 王登红, 等. 中国成矿区带划分方案[M]. 北京: 地质出版社, 2008.
[16] Xu Z G, Chen Y C, Wang D H, et al. The scheme of the classification of the minerogenetic units in China[M]. Beijing: Geological Publishing House, 2008.
[17] Sun S S, Mcdonough W F. Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J]. Geological Society London Special Publications, 1989, 42(1):313-345.
doi: 10.1144/GSL.SP.1989.042.01.19
[18] 赵彦彦, 郑永飞. 碳酸盐沉积物的成岩作用[J]. 岩石学报, 2011, 27(2):501-519.
[18] Zhao Y Y, Zheng Y F. Diagenesis of carbonate sediments[J]. Acta Petrologica Sinica, 2011, 27(2):501-519.
[19] 曹俊臣. 中国矿床[M]. 北京: 地质出版社, 1994:314-340.
[19] Cao J C. Mineral deposits of China[M]. Beijing: Geological Publishing House, 1994:314-340.
[20] 朱敬宾, 王吉平, 商朋强, 等. 中国萤石矿床锶同位素、氢氧同位素地球化学特征.[J]. 化工矿产地质, 2021, 43(1):7-16.
[20] Zhu J B, Wang J P, Shang P Q, et al. Geochemical characteristics of strontium and hydrogen and oxygenisotopes in fluorite deposits in China[J]. Geology of Chemical Minerals, 2021, 43(1):7-16.
[21] 河南地质矿产厅. 云阳幅、四里店幅1∶5万区域地质调查报告[R]. 河南地质矿产厅,1989.
[21] Henan Department of Geology and Mineral Resources. Yunyang sheet and Silidian sheet 1∶50,000 regional geological survey report[R] .Henan Department of Geology and Mineral Resources,1989.
[22] Barbieri M, Tolomeo L, VotTbiggio M. Yttrium,lanthanum and manganese geochemistry in fluorite deposits from Sardinia(Italy)[J]. Chemical Geology, 1983, 40:43-50.
doi: 10.1016/0009-2541(83)90090-6
[23] 吴益平, 张连昌, 袁波, 等. 新疆阿尔金地区卡尔恰尔超大型萤石矿床地质特征及成因[J]. 地球科学与环境学报, 2021, 43(6):962-977.
[23] Wu Y P, Zhang L C, Yuan B, et al. Geological characteristics and genedis of the super-large Kalqiar fluorite deposit in Altyn Tagh Area of Xinjiang,China[J]. Journal of Earth Sciences and Environment, 2021, 43(6):962-977.
[24] 张凯涛, 白德胜, 李俊生, 等. 豫西合峪—车村地区萤石矿床地质特征及物质来源研究进展[J]. 物探与化探, 2022, 46(4):787-797.
[24] Zhang K T, Bai D S, Li J S, et al. Research progress in the geological characteristics and material sources of fluorite deposits in the Heyu-Checun area,western Henan Province[J]. Geophysical and Geochemical Exploration, 2022, 46(4):787-797.
[25] 冯绍平, 汪江河, 刘耀文, 等. 豫西杨山萤石矿稀土元素地球化学特征及其指示意义[J]. 稀土, 2020, 41(5):50-58.
[25] Feng S P, Wang J H, Liu Y W, et al. Geochemistry characteristics of rare earth elements in Yangshan fluorite deposit,western Henanand their indicative significance[J]. Rare Earth, 2020, 41(5):50-58.
[26] 孙海瑞, 黄智龙, 周家喜, 等. 热液矿床中萤石的稀土元素地球化学及其地质意义[J]. 岩石矿物学杂志, 2014, 33(1):185-193.
[26] Sun H R, Huang Z L, Zhou J X, et al. Rare earth elements geochemistry of fluorite in hydrothermal deposits and its geological significance[J]. Acta Petrologica et Mineralogica, 2014, 33(1):185-193.
[27] 朱江, 彭三国, 刘锦明. 西大别地区白垩纪灵山花岗岩基外围发现萤石矿点[J]. 中国地质, 2020, 47(2):550-551.
[27] Zhu J, Peng S G, Liu J M. The discovery of fluorite ore spots in the contact zone of Cretaceous Lingshan granitic batholith in the western Dabie orogenic belt[J]. Geology in China, 2020, 47(2):550-551.
[28] Bau M, Dulski P. Comparativestudy of yttrium and rare-earth element behaviours in fluouine-richhydouthermalfluids[J]. Contribution to Mineralogy and Petrology, 1995, 119(2):213-223.
doi: 10.1007/BF00307282
[29] Ismail I, Baioumy H, Ouyang H, et al. Origin of fluorite mineralizations in the Nuba Mountain,Sudan and their rare earth element geochemistry[J]. Journal of African Earth Sciences, 2015, 112:276-286.
doi: 10.1016/j.jafrearsci.2015.09.016
[30] 许东青, 聂凤军, 钱明平, 等. 苏莫查干敖包超大型萤石矿床的稀土元素地球化学特征及其成因意义[J]. 矿床地质, 2009, 28 (1):29-41.
[30] Xu D Q, Nie F J, Qian M P, et al. REE geochemistry and genesis of Sumochagan Obo superlarge fluorite deposit[J]. Mineral Deposits, 2009, 28(1): 29-41.
[31] 邹灏, 方乙, 陈合毛, 等. 浙江天台盆地下陈萤石矿稀土元素地球化学特征及成因[J]. 中国地质, 2014, 41(4):1375-1386.
[31] Zou H, Fang Y, Chen H M, et al. REE geochemistry and genesis of the Xiachen fluorite deposit in Tiantai basin,Zhejiang Province[J]. Geology in China, 2014, 41(4):1375-1386.
[32] 张青松, 王春连, 栗克坤, 等. 闽北大坪萤石矿构造蚀变、岩石地球化学特征与矿床成因探讨[J]. 岩石矿物学杂志, 2021, 40(6):1131-1140.
[32] Zhang Q S, Wang C L, Li K K, et al. Discussion on structural alteration rock geochemistry characteristics and genesis of Daping fluorite deposit in northern Fujian[J] Acta Petrologica Et Mineralogica, 2021, 40 (6):1131-1140.
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