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XI Zhixuan, WANG Chen, BIAN Jiahua, JI Xiang, FENG Wei. 2020. Metallogenic Epoch Characteristics and Geochemical Features of Granitic Pegmatite Rare Earth Ore in Tabutou Area, Shandong Province. Northwestern Geology, 53(3): 10-40. doi: 10.19751/j.cnki.61-1149/p.2020.03.002
Citation: XI Zhixuan, WANG Chen, BIAN Jiahua, JI Xiang, FENG Wei. 2020. Metallogenic Epoch Characteristics and Geochemical Features of Granitic Pegmatite Rare Earth Ore in Tabutou Area, Shandong Province. Northwestern Geology, 53(3): 10-40. doi: 10.19751/j.cnki.61-1149/p.2020.03.002
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Metallogenic Epoch Characteristics and Geochemical Features of Granitic Pegmatite Rare Earth Ore in Tabutou Area, Shandong Province

  • 1. Northwest Nonferrous Survey Engineering Company, Xi'an 710054, Shaanxi, China;

  • 2. Shaanxi Provincial Department of Natural Resources, Xi'an 710082, Shaanxi, China;

  • 3. Henan Aerial Geophysical Remote Sensing Center, Zhengzhou 450000, Henan, China;

  • 4. Jiaozuo Earthquake Station, Henan Province, Jiaozuo 454000, Henan, China;

  • 5. Northwest Highway Research Institute, Xi'an 710025, Shaanxi, China

Received Date:  30 September 2019
Revised Date:  02 June 2020
    Abstract
  • Based on the field investigation and the division of pegmatite belts, through the analysis of petrography, isotope chronology, and geochemistry, the authors determined the diagenetic and metallogenic age and discussed the source of ore-forming material and the relationship between pegmatite and rare earth ore to establish a metallogenetic model of the deposit.The geochemical characteristics show that the rare earth-bearing pegmatite is low silicon, low alkali and iron peraluminous-rich. potassium chang-plagioclase granite pegmatite, potash feldspathic granite pegmatite and potash feldspar granite all have the characteristics of high silicon and alkali and low iron peraluminous. There is a clear differentiation of light and heavy rare earth element, a loss of high field-strength elements such as Ta, Ti, Nb and P, and an enrichment of large ion lithophiles elements as K and Rb. The LA ICP-MS isotope dating shows that the Th-Pb dating of the bastnasite was(128.5±2.0) Ma and (134.4±1.2) Ma, indicating that the mineralization of rare earth occurred in Mesozoic Cretaceous.
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  • 李建康. 川西典型伟晶岩型矿床的形成机理及其大陆动力学背景[D]. 北京:中国地质大学, 2006.

    Google Scholar

    LI Jiankang. Formation mechanism and continental dynamics background of typical pegmatite deposits in western Sichuan[D]. Beijing:China University of Geosciences, 2006.

    Google Scholar

    徐新文. 青海省铌钽矿类型、特征及找矿方向[J]. 西部探矿工程, 2009,3:144-147.

    Google Scholar

    XU Xinwen. Types, characteristics and prospecting direction of niobium and tantalum deposits in Qinghai Province[J]. Westward Exploration Engineering, 2009, 3:144-147.

    Google Scholar

    邹天人, 徐建国.论伟晶岩的成因和类型的划分[J]. 地球化学, 1975 (3):161-174.

    Google Scholar

    ZOU Tianren, XU Jianguo. On the formation and types of pegmatite[J]. Geochemistry, 1975 (3):161-174.

    Google Scholar

    杨守业, 李从先. REE示踪沉积物物源研究进展[J]. 地球科学进展, 1999, 14 (2):164-167.

    Google Scholar

    YANG Shouye, LI Congxian. REE Tracer Sediment Source Research Progress[J]. Advances in Earth Science, 1999, 14 (2):164-167.

    Google Scholar

    陈西京. 深处岩浆分异与某地花岗伟晶岩的形成[J]. 地球化学, 1976, 3:213-219.

    Google Scholar

    CHEN Xijing. Magmatic differentiation in deep and the formation of granite pegmatite in a certain place[J]. Geochemistry, 1976, 3:213-219.

    Google Scholar

    袁见齐, 朱上庆, 翟裕生. 矿床学[M]. 北京:地质出版社, 1985:54-71.

    Google Scholar

    YUAN Jianqi, ZHU Shangqing, ZHAI Yusheng. Mineral Deposits[M]. Beijing:Geological Publishing House, 1985:54-71.

    Google Scholar

    王贤觉,邹天人.阿尔泰伟晶岩矿物研究[M].北京:科学出版社,1981.

    Google Scholar

    WANG Xianjue, ZOU Tianren. Altai Pegmatite Mineral Research[M]. Beijing:Science Press, 1981.

    Google Scholar

    邹天人, 李庆昌. 中国新疆稀有稀土金属矿床[M]. 北京:地质出版社,2005:111-138.

    Google Scholar

    ZOU Tianren, LI Qingchang. Rare rare earth metal deposits in Xinjiang, China[M]. Beijing:Geological Publishing House,2005:111-138.

    Google Scholar

    邹天人, 杨岳清. 中国两源伟晶岩的成矿作用[A]. 国际交流地质学术文集-为二十七届国际地质大会撰写[C].北京:地质出版社, 1984, (3):161-174.

    Google Scholar

    ZOU Tianren, YANG Yueqing. The mineralization of China's two-source pegmatites[A]. International exchange of geological academic papers-written for the 27th International Geological Congress[C]. Beijing:Geological Publishing House, 1984, (3):161-174.

    Google Scholar

    陈毓川, 薛春纪, 王登红, 等. 华北陆块北缘区域矿床成矿谱系探讨[J], 高校地质学报, 2003,9(4):520-535.

    Google Scholar

    CHEN Yuchuan, XUE Chunji, WANG Denghong, et al. 2003. Discussion on metallogenic genealogy of regional deposits in the northern margin of the North China continental block[J], Journal of University Geology, 9 (4):520-535.

    Google Scholar

    李靖辉. 豫西卢氏产铀伟晶岩地质特征及其找矿前景分析[J]. 华东理工大学学报(白然科学版), 2010,33(3) 257-261.

    Google Scholar

    LI Jinghui. Geological characteristics and prospecting analysis of uranium-produced pegmatite from Lu's in western Henan[J]. Journal of East China University of Science and Technology (Bairan Science Edition), 2010,33 (3) 257- 261.

    Google Scholar

    屈敏, 郭敬辉, 赖勇, 等. 华北克拉通中部带高压麻粒岩地体中1.81Ga富钡冰长石伟晶岩脉的成因及地质意义[J]. 中国科学:地球科学, 2011. 41(12):1840-1850.

    Google Scholar

    QU Min, GUO Jinghui, LAI Yong, et al. Genesis and geological significance of the 1.81Ga barium-rich ice-feldspar pegmatite vein in the high-pressure granulite terrane in the central belt of the North China Craton[J]. Science in China:Earth Science, 2011. 41 (12):1840-1850.

    Google Scholar

    金景福. 中国东南部中生代含铀花岗岩成矿物质来源与铀成矿作用[J]. 岩矿测试. 1984,3:112-119.

    Google Scholar

    JIN Jingfu. Source of mineralization materials and uranium mineralization of Mesozoic uranium-bearing granite in southeastern China[J]. Rock and Mineral Testing. 1984,3:112-119.

    Google Scholar

    李兆麟. 关于变质深熔作用与成岩成矿关系的思考[J]. 地学前缘, 2001,8(3):29-38.

    Google Scholar

    LI Zhaolin. Thoughts on the relationship between metamorphism and deep melting and diagenesis and mineralization[J]. Earth Science Frontiers, 2001, 8 (3):29-38.

    Google Scholar

    李兆麟, 杨荣勇, 李文, 等. 中国不同成因伟晶岩形成的物理化学条件[J]. 地质科技情报, 1998,17:29-34.

    Google Scholar

    LI Zhaolin, YANG Rongyong, LI Wen, et al. 1998. Physical and chemical conditions for the formation of pegmatites of different origins in China[J]. Geological Science and Technology Information, 1998, 17:29-34.

    Google Scholar

    王登红, 邹天人, 李红阳. 稀有金属经济地质研究进展[J]. 地质科技情报, 1998, 17(3):63-68.

    Google Scholar

    WANG Denghong, ZOU Tianren, LI Hongyang. Advances in economic geology research of rare metals[J]. Geological Science and Technology Information, 1998, 17 (3):63-68.

    Google Scholar

    刘福来, 王舫, 刘平华. 北苏鲁威海地区伟晶岩的形成过程及其与超高压岩石深熔作用的成因关系[J]. 地质学报, 2009,83(11):1689-1702.

    Google Scholar

    LIU Fulai, WANG Fang, LIU Pinghua. The formation process of pegmatite in the Weihai area of North Sulu and its genetic relationship with ultrahigh-pressure rock deep melting[J]. Acta Geologica Sinica, 2009,83 (11):1689-1702.

    Google Scholar

    王继芳, 孙茂田. 山东省郗山稀土矿地质特征及找矿前景分析[J]. 山东国土资源,2016(6):32-40.

    Google Scholar

    WANG Jifang, SUN Maotian. Geological characteristics and prospecting analysis of Xishan rare earth deposit in Shandong Province[J]. Shandong Land and Resources, 2016 (6):32-40.

    Google Scholar

    王辰,刘建朝,张海东,等. 山东省微山碳酸盐岩年代学、矿物学[J]. 地学前缘,2019(10):769-785.

    Google Scholar

    WANG Chen, LIU Jianchao, ZHANG Haidong, et al. Geochronology and mineralogy of the Weishan carbonatite in Shandong province, eastern China[J]. Geoscience Frontiers,2019(10):769-785.

    Google Scholar

    汪子杰, 徐晓慧. 莱西塔埠头稀土矿氟碳铈矿Th-Pb定年及矿床成因[J]. 山东国土资源, 2018,34(10):62-66.

    Google Scholar

    WANG Zijie, XU Xiaohui. Th-Pb dating and deposit genesis of the fluorescerite deposit in the Tabutou rare earth mine in Laixi[J]. Shandong Land and Resources, 2018, 34 (10):62-66.

    Google Scholar

    李洪奎, 杨永波. 山东重大基础地质问题研究进展[J]. 岩石学报, 2013, 29(2):594-606.

    Google Scholar

    LI Hongkui, YANG Yongbo. Research progress of major basic geological problems in Shandong[J]. Acta Petrologica Sinica, 2013, 29 (2):594-606.

    Google Scholar

    李洪奎, 杨永波. 山东大地构造相研究方法划分方案与基本特征[J]. 山东国土资源, 2014, 30(4):1-12.

    Google Scholar

    LI Hongkui, YANG Yongbo. Division scheme and basic characteristics of Shandong tectonic facies research method[J]. Shandong Land and Resources, 2014, 30 (4):1-12.

    Google Scholar

    李明春, 李三忠. 中国胶东焦家式金矿类型及其成矿理论[J]. 吉林大学学报, 2014, 44(1):87-104.

    Google Scholar

    LI Mingchun, LI Sanzhong. Jiaojia-style gold deposits in Jiaodong, China and their metallogenic theory[J]. Journal of Jilin University, 2014, 44 (1):87-104.

    Google Scholar

    邹天人, 李庆昌. 中国新疆稀有稀土金属矿床[M]. 北京:地质出版社, 2005:111-138.

    Google Scholar

    ZOU Tianren, LI Qingchang. Rare rare earth metal deposits in Xinjiang, China[M]. Beijing:Geological Publishing House, 2005:111-138.

    Google Scholar

    邹天人, 杨岳清. 中国两源伟晶岩的成矿作用[C]. 国际交流地质学术文集,1984.

    Google Scholar

    ZOU Tianren, YANG Yueqing. The metallogenesis of China's two-source pegmatite[C]. International Exchange Geological Academic Collection, 1984.

    Google Scholar

    李三忠, 赵国春, 孙敏. 华北克拉通早元古代拼合与Columbia超大陆形成研究进展[J]. 力学通报, 2016, 61(9):919-925.

    Google Scholar

    LI Sanzhong, ZHAO Guochun, SUN Min. Advances in the Early Proterozoic Combination of North China Craton and the Formation of Columbia Supercontinent[J]. Mechanics Bulletin, 2016, 61 (9):919-925.

    Google Scholar

    夏林祈. 超大陆构造、地幔动力学和岩浆-成矿响应[J]. 西北地质, 2013, 46 (3):1-38.

    Google Scholar

    XIA Linqi. Supercontinental structure, mantle dynamics and magmatic-metallogenic response[J]. Northwestern Geology, 2013, 46 (3):1-38.

    Google Scholar

    涂光炽. 试论非常规超大型矿床物质组成、地质背景、形成机制的某些独特性-初谈非常规超大型矿床[J]. 中国科学:地球科学, 1998, 28(s2):1-6.

    Google Scholar

    TU Guangzhi. On the uniqueness of the material composition, geological background, and formation mechanism of unconventional super-large deposits-A preliminary discussion on unconventional super-large deposits[J]. Chinese Science:Earth Science, 1998, 28 (s2):1-6.

    Google Scholar

    李献华, 李武显, 何斌. 华南陆块的形成与Rodinia超大陆聚合-裂解-观察、解释与检验[J]. 矿物岩石地球化学通报, 2012, 16(2):543-559.

    Google Scholar

    LI Xianhua, LI Wuxian, HE Bin. Formation of South China Continent and Rodinia Supercontinent Aggregation-Cracking-Observation, Interpretation and Inspection[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2012, 16 (2): 543-559.

    Google Scholar

    董正阁, 丹增卓玛. 关于超级大陆旋回的探讨[J]. 科技创新与应用, 2016, 8(28):35-36.

    Google Scholar

    DONG Zhengge, DANZENG Zhuoma. Discussion on Super Continental Cycle[J]. Science and Technology Innovation and Application, 2016, 8 (28):35-36.

    Google Scholar

    李献华, 王选策, 李武显, 等. 华南新元古代玄武质岩石成因与构造意义:从造山运动到陆内裂谷[J]. 地球化学. 2008(04):382-392.

    Google Scholar

    LI Xianhua, WANG Xuance, LI Wuxian, et al. Genesis and tectonic significance of Neoproterozoic basalt rocks in South China:from orogeny to intracontinental rift[J]. Geochemistry. 2008 (04):382-392.

    Google Scholar

    温利刚, 曾普胜, 詹秀春, 等. 迤纳厂矿床:一个"白云鄂博式"铁-铜-稀土矿床[J]. 地学前缘, 2018, 9(28):1-26.

    Google Scholar

    WEN Ligang, ZENG Pusheng, ZHAN Xiuchun, et al. Yinnachang deposit:a "Baiyun Ebo style" iron-copper-rare earth deposit[J]. Earth Science Frontiers, 2018, 9 (28):1-26.

    Google Scholar

    赵振华, 王中刚, 邹天人, 等. 新疆乌伦占富碱侵入岩成因讨论[J]. 地球化学, 1996, 25(3):205-220.

    Google Scholar

    ZHAO Zhenhua, WANG Zhonggang, ZOU Tianren, et al. Discussion on the genesis of alkali-rich intrusive rocks in Wulunzhan, Xinjiang[J]. Geochemistry, 1996, 25 (3):205-220.

    Google Scholar

    夏明哲, 姜常义, 钱壮志, 等. 新疆东天山葫芦岩体岩石学与地球化学研究[J]. 岩石学报, 2008, 24(12):2749-2760.

    Google Scholar

    XIA Mingzhe, JIANG Changyi, QIAN Zhuangzhi, et al. Petrology and geochemistry of the gourd rock mass in Dongtian Mountain, Xinjiang[J]. Acta Petrologica Sinica, 2008, 24 (12):2749-2760.

    Google Scholar

    夏昭德. 新疆北山地区笔架山岩带镁铁一超镁铁质岩体岩石成因研究[D]. 西安:长安大学博士论文, 2012.

    Google Scholar

    XIA Zhaode. Research on the rock genesis of the mafic-ultramafic rock mass in Bijiashan rock belt in Beishan area, Xinjiang[D]. Xi'an:Doctoral Dissertation of Chang'an University, 2012.

    Google Scholar

    李献华, 周汉文, 韦刚健,等.滇西新生代超钾质煌斑岩的元素和Sr-Nd同位素特征及其对岩石圈地幔组成的制约[J]. 地球化学, 2002, 3(1):26-35.

    Google Scholar

    LI Xianhua, ZHOU Hanwen, WEI Gangjian, et al. Elemental and Sr-Nd isotope characteristics of Cenozoic superpotassic porphyry in western Yunnan and their constraints on lithospheric mantle composition[J]. Geochemistry, 2002, 3 (1):26-35.

    Google Scholar

    BENDER E. F, ANDERSON J. I. Nature and origin oI Protcrozoic A-type granitic magmatism in the southwestern United States of America[J]. Lithos, 1989, (23):19-52.

    Google Scholar

    CONDIE K. C. Plate tectonics and rrustal evolution(2nd edition)[M]. Perga Mnz Press, 1982.

    Google Scholar

    CERNY P. Fertile granites of Precambrian rare-element pegmatite fields:is geochemistry controlled by tectonic setting or source lithologier[J]. Precambrian Research, 1991a, 51:429-468.

    Google Scholar

    CONDIE K. C. Breakup of a Paleoproterozoic supercontinent[J]. Gondwana Research, 2002, 5(1):41-43.

    Google Scholar

    EVENSEN, J. M, LONDON, D. Experimental silicate mineral/melt pertition coefficients for beryllium and the beryllium cycle from migmatite to pegmatite geochim[J]. Cosrnochim Acta.,2002,66:2239-2265.

    Google Scholar

    DICKIN A. P. Nd isotope chemistry of Tertiary igneous rocks from Arran, Scotland:Implications for magma evolution and crustal structure[J]. Geol Mag, 1994, (131):329-333.

    Google Scholar

    FARMER G L, PERRY F. V, SEMKEN S, et a1. Isotopic evidence on the structure and origin of subcontinental lithospheric mentle in Southern Nevada[J]. Journal of Geophysical Research, 1989, 94:7885-7898.

    Google Scholar

    HOU G. T, SANTOSH M, QIAN X. L, et al. Configuration of the late Paleoproterozoic supercontinent Columbia:Insights from radiating mafic dyke swarms[J]. Gondwana Research, 2008, 14(3):395-409.

    Google Scholar

    LI Z. X, LI X. H, ZHOU H. W, et al. Grenvillian continental collision in south China:New SHRIMP U-Pb Zrncon results and implications for the configuration of Rodinia[J]. Geology, 2002, 30(2):163-166.

    Google Scholar

    LI H. K, LU S. N, SU W. B, et al. Recent advances in the study of the Mesoproterozoic geochronology in the North China Craton[J]. Journal of Asian Earth Sciences, 2013, 72(10):216-227.

    Google Scholar

    LONDON D, HERVIG R L, MORGAN G B VI. Melt-vapor solubilities and elemental partitioning in peraluminous granite-pegmatite systems:experimental results with Macusani glass at 200Mpa[J]. Contrib Mineral Petrol, 1988, 99:360-373.

    Google Scholar

    LONDON, D. Granitic pegmatites:an assessment of current concept and direction for future[J]. Lithos, 2005,80:281-303.

    Google Scholar

    PLANK T. The brine of the Earth[J]. Nature, 1996, 380:202-203.

    Google Scholar

    ROGERS J. J. W, SANTOSH M. Configuration of Columbia, a Mesoproterozoic supercontinent[J]. Gondwana Research, 2002, 5(1):5-22.

    Google Scholar

    ROGERS J. J. W, SANTOSH M. Tectonics and surface effects of the supercontinent Columbia[J]. Gondwana Research, 2009, 15(3):373-380.

    Google Scholar

    SANTOSH M, MARUYAMA S, YAMAMOTO S. The making and breaking of supercontinents:Some speculations based on superplumes, super downwelling and the role of tectosphere[J]. Gondwana Research, 2009, 15(3):324-341.

    Google Scholar

    SHEARER, C.K., PAPIKE, J. J. Petrogenetic links aMnzg granites and pegmatites in the Harney Peak rear-element granite-pegmatite system, Black Hills, south Dakota. Can Mineral,1992,30:785-809.

    Google Scholar

    SKUBLOV S, ASTAF'EV B, MARIN Y, et al. First find of cerianite in Zrncons from metasomatites of the Terskii greenstone belt, Baltic shield[J]. Doklady Earth Sciences, 2009, 428(1):1134-1138.

    Google Scholar

    XIONG X, KEPPLER H, AUDETAT A, et al. Partitioning of Nb and Ta between ruble and felsic melt and the fractionation of Nb/Ta during partial melting of hydrous metabasalt[J]. Geochimica et Cosmochimica Acta, 2011, 75(7):1673- 1692.

    Google Scholar

    XIONG X. L,ADAM J,GREEN T. H. Ruble stability and ruble/melt HFSE partitioning during partial melting of hydrous basalt:Implications for TTG genesis[J].Chemical Geology, 2005, 218(3-4):339-359.

    Google Scholar

    YANG J. H,WU F. H, CHUNG S. I, et al. A hybrid origin for the Qians-han A-type granite,northeast China:Geochemical and Sr-Nd-Hf isotopic evidence[J]. Lithos, 2006, (89):89-106.

    Google Scholar

    XI A. L. Q, XIA Z. C, XU X. Y, et al. Mid-Late Neoproterozoic rift-related volcanic rocks in China:Geological records of rifting and break-up of Rodinia[J]. Geoscience Frontiers, 2012, 3(4):375-399.

    Google Scholar

    ZHAO G. C, SUN M, WILDE S. A, et al. A Paleo-Mesoproterozoic supercontinent:Assembly, growth and breakup[J]. Earth Science Reviews, 2004,67(1/2):91-123.

    Google Scholar

    ZHAO G. C, SUN M, WILDE S. A, et al. Assembly, accretion and breakup of the Paleo-Mesoproterozoic Columbia supercontinent:Records in the North ChinaCraton[J]. Gondwana Research, 2003, 6(3):417-434.

    Google Scholar

    ZHAO G. C, CAWOOD P. A, WILDE S. A, et al. Review of global 2.1-1.8Ga orogens:Implications for a pre-Rodinia supercontinent[J]. Earth-Science Reviews, 2002, 59(1/2/3/4):125-162.

    Google Scholar

    TU Guangzhi. Some advances in the study of solid geology and ultra-large deposits in the 1990s[J]. Journal of Mineralogy, 1997, 17 (4):357-363.

    Google Scholar

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