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物探与化探  2022, Vol. 46 Issue (1): 46-57    DOI: 10.11720/wtyht.2022.1040
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
华北地区稀土矿床特征及找矿方向
赵泽霖1(), 李俊建1(), 张彤2, 倪振平3, 彭翼4, 宋立军5
1.中国地质调查局 天津地质调查中心,天津 300170
2.内蒙古自治区地质调查院,内蒙古 呼和浩特 010020
3.山东省地质调查院, 山东 济南 250013
4.河南省地质调查院,河南 郑州 450007
5.河北省地质调查院,河北 石家庄 050081
Geological characteristics and prospecting direction of rare earth element deposits in North China
ZHAO Ze-Lin1(), LI Jun-Jian1(), ZHANG Tong2, NI Zhen-Ping3, PENG Yi4, SONG Li-Jun5
1. Tianjin Center of China Geological Survey,Tianjin 300170,China
2. Inner Mongolia Autonomous Institute of Region Geological Survey,Hohhot 010020,China
3. Shandong Institute of Geological Survey,Jinan 250013,China
4. Henan Institute of Geological Survey,Zhengzhou 450007,China
5. Hebei Provincial Bureau of Geological Survey,Shijiazhuang 050081,China
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摘要 

在系统收集华北地区稀土矿床资料基础上,分析了华北地区稀土资源现状及稀土矿床的时间、空间分布规律。分析认为,华北地区稀土矿床成矿类型主要包括沉积变质型、火成碳酸岩浆型、岩浆热液型、伟晶岩型和离子吸附型。根据华北地区稀土矿床构造位置及控矿特征,认为华北地区古老变质基底、太古宙—古元古代陆块边缘裂谷带、中元古代陆缘裂谷带、燕山期滨西太平洋活动陆缘均是稀土矿床成矿的有利地球动力学背景。区域深大断裂、地槽发育初期的火山—沉积事件及碱性正长岩和碱性花岗岩类岩浆活动,是寻找各类稀土矿床的有利构造—沉积—岩浆条件,降雨量高、冲积平原、棕壤—褐土分布区则提供良好的稀土元素地球化学背景。

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赵泽霖
李俊建
张彤
倪振平
彭翼
宋立军
关键词 华北板块及周缘稀土矿床成因类型找矿方向    
Abstract

Based on the systematic collection of information of rare earth element (REE) deposits in North China, this paper analyzes the current situation of REE resources and the temporal-spatial distribution regulation of REE deposits in North China.The mineralization types of the REE deposits in North China mainly include sedimentary and metamorphic type, igneous carbonate magma type, magmatic hydrothermal type, pegmatite type, andion-adsorption type. Given thegeotectonic locations and ore-controlling factorsof REE deposits in North China, the geodynamic background favorable for the formation of the REE deposits includes the ancient metamorphic basement, Archean-Paleoproterozoic rift zones on continental margins, Middle Proterozoic rift zoneson continental margins, and Yanshanian active continental margins in coastal areas of the West Pacific. Thetectonic-sedimentary-magmatic prospecting favorable conditions include volcanic-sedimentary events during the early development of regional deep faults and geosynclines and the magmatic activitiesof alkaline syenitesand alkaline granites. Meanwhile, the geochemical background favorable for REE mineralization consists of high precipitation amount, alluvial plains, and brown soil distribution areas.

Key wordsNorth China Plate and its periphery    rare earth element deposits    mineralization type    prospecting direction
收稿日期: 2021-01-20      修回日期: 2021-05-24      出版日期: 2022-02-20
ZTFLH:  P632  
基金资助:中国地质调查局项目(DD20190379-31);中国地质调查局项目(1212011121029);中国地质调查局项目(200110200038);国家重点研发计划“深地资源勘查开采”重点专项课题(2016YFC0600107);国家重点研发计划“深地资源勘查开采”重点专项课题(2018YFC0603805-1)
通讯作者: 李俊建
作者简介: 赵泽霖(1991-),男,硕士,工程师,主要从事区域地质调查和成矿作用研究工作。Email: tishan_yuei@163.com
引用本文:   
赵泽霖, 李俊建, 张彤, 倪振平, 彭翼, 宋立军. 华北地区稀土矿床特征及找矿方向[J]. 物探与化探, 2022, 46(1): 46-57.
ZHAO Ze-Lin, LI Jun-Jian, ZHANG Tong, NI Zhen-Ping, PENG Yi, SONG Li-Jun. Geological characteristics and prospecting direction of rare earth element deposits in North China. Geophysical and Geochemical Exploration, 2022, 46(1): 46-57.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2022.1040      或      https://www.wutanyuhuatan.com/CN/Y2022/V46/I1/46
Fig.1  华北地区稀土矿分布(据文献[22]修改)

成矿
类型
矿区地质特征 矿体特征 矿石特征

白云鄂博稀土矿 火成
碳酸
岩型
出露中元古界下白云鄂博群和石炭系宝力格庙组火山岩。白云鄂博群包括17个岩性段(H1-H17)和6个岩组,其中H8白云质大理岩是主要的铌—稀土—铁矿体主要赋矿层位,H9为板岩,为矿体顶板,呈断层接触。矿区侵入岩包括古元古代片麻状斜长片麻岩和海西期闪长质—花岗质岩类,与矿化无关。矿区褶皱发育,作用于白云鄂博群各岩性段,H1、H2为宽沟北向核部,H9、H10为白云向斜核部。矿区北部为白银角拉克—宽沟断裂,为EW走向并与乌兰布拉格大断裂交汇,交汇处控制了白云岩产出 矿体包括主矿、东矿、西矿和东部接触带4个矿区。东矿产于白云向斜北翼,NEE走向,倾向SSW,长1 300 m,宽均179 m,最大延伸深870 m,呈不规则透镜体状,两端渐变成白云岩及板岩;主矿体位于白云向斜南翼,走向近EW向,倾向S,长1 250 m,平均宽245 m,最大延伸深度 1 030 m,呈透镜体状,两端尖火于白云岩中。西矿矿段为主矿以西由东西向排列十数个小矿体组成,东西长10 km,南北宽约1 km,呈层状、透镜状,具条带状构造,铁矿体与围岩界限不清,由品位圈定。东部接触带位于白云向斜构造的北冀,白云岩与海西期花岗岩接触部位处。矿体产状多与围岩产状一致,总体呈透镜体、层状和似层状 矿石具有粒状变晶结构、粉尘状结构、交代结构、固溶分离结构等;具块状构造、浸染状构造、条带状构造、层纹状构造、斑杂状构造、角砾状构造等。主要有用元素为铁、铌、稀土,其次含多种分散元素和放射性元素。造岩矿物为白云石、方解石和石英等。稀土矿物主要为独居石、氟碳铈矿、黄河矿、氟碳钙铈矿和磷耿石等。含铁矿物为磁铁矿和赤铁矿。主要含铌矿物为铌铁矿、易解石 、褐钇铌矿、烧绿石和铌铁金红石等。铁矿储量1 500 Mt(35%Fe),REE储量48 Mt(6%RE2O3)和1 Mt Nb (0.13% Nb) 超大型 中元古代
郗山轻稀土矿 碱性
岩浆
岩型
出露太古宇泰山群山草峪组黑云斜长片麻岩。燕山期花岗岩发育,受微山湖—东平湖断裂控制。含矿碱性杂岩体主为正长岩、石英正长岩、霓辉石英正长岩,呈椭圆形,NW-SE向延伸,SW向倾斜,侵于山草峪组。控矿构造和容矿构造为EW向、NNW向、NE向、NEE向、SN向和EW向6组断裂 矿体包以萤石型矿脉、石英重晶石型矿脉和石英方解石型矿脉形式产出,括矿脉60余条,多分布在碱性岩体顶、底板附近。单条矿脉长110~580 m,深200~500 m,宽0.2~8 m。矿脉由氟碳铈矿、萤石、重晶石、石英、方解石等组成。矿脉多充填于北西向压扭性构造裂隙中,倾向210~245°,倾角50°~70° 稀土矿物主为氟碳铈矿、氟碳钙铈矿、铈磷灰石、铈镧霓辉石,次为锆英石、褐帘石、独居石、榍石等。主要有益组分为轻稀土元素,包括Ce、La、Nd、Pr、Sm以及Eu、Er、Gd、Lu、Y 等;其他金属元素有Tu、U、Mo、Pb等。TR2O3变化于1.55%~4.92%,平均3.25% 中型 燕山晚期
桃花拉山稀有稀土矿 沉积
变质
矿区出露前中元古界二道凹群中深变质岩系,含矿层位为条带状大理岩夹角闪片岩、薄层状钙质片岩。与矿体接触处多为薄层状,颜色变暗,颗粒渐次变细。侵入岩主要包括吕梁期闪长岩和加里东晚期花岗岩。成矿前断裂为走向310°~315°,大体呈“S”形,中间近东西,为控矿的主要构造。成矿后断裂对矿体起破坏作用 矿带东西长达11 km,南北宽约60 m,走向295°~310°,南倾,倾角60°~75°。目前大致圈出20个矿体(西矿区12个,东矿区8个),长35~904 m,多数为200~500 m。平均厚1.4~14.0 m,延深一般在200 m以下。矿体多为似层状,少数呈透镜状。矿层与围岩呈渐变关系,并可见同步褶皱现象,局部为断层接触。围岩一般为条带状大理岩,局部地段的围岩为花岗质混合岩 矿石自然类型分为大理岩型和片岩型。主要工业矿物为铌铁矿、铁铁金红石、独居石、易解石等。矿石结构为不等粒花岗变晶结构、花岗变晶结构、花岗鳞片变晶结构,矿石构造有块状构造、片状构造。与铌、稀土、磷矿化有关的蚀变主要为褐铁矿化、黑云母化、磷酸盐化、钾钠长石化 中型 古元古代
塔埠头稀土矿 伟晶
岩型
矿区出露地层主要为古元古界荆山群野头组,岩性为黑云变粒岩、大理岩、斜长角闪岩等,总体走向近EW向。矿区侵入岩主要为燕山晚期花岗岩、花岗伟晶岩、石英脉,稀土矿化主要发育在花岗伟晶岩中。断裂构造主要有近EW向的上庄断裂及水集—徐格庄断裂 共探明4个工业矿体,稀土氧化物总储量398 t,平均品位1.603%,主要包含4个矿体[38],矿体呈似层状或板状,长33.5~60 m,平均厚1.57~7.47 m,延伸7~43 m,倾向为NNE,倾角32°~68° 矿石矿物包括褐帘石、氟碳铈镧矿、锆石、榍石、钍石等;脉石矿物主要有钾长石、斜长石、石英、黑云母等。矿石中稀土元素含量较高,主要为铈、镧、钕、钇等,铌、钍均达到工业要求,另含一定量的铀、钽、铪、铷、铯等有用元素 小型 燕山期
东七一山稀有矿 碱性
岩浆
岩型
矿区出露寒武—奥陶系西双鹰山组碎屑岩夹火山岩。侵入岩为七一山复式杂岩体,其中含矿岩体为碱长花岗斑岩和似斑状碱长花岗岩,局部或外围见石英闪长岩、花岗闪长岩、二云母花岗岩、黑云母花岗岩等 52 号铷矿体分布在钠长石化花岗岩中。走向NE—SW向,倾向N。为一简单透镜体,长400 m,厚172. 5 m。铍矿体含铍矿物为细粒绿柱石,脉石矿物为钠长石、石英、黄玉、铁锂云母等 铷矿体见于钠长石化花岗岩中,元素赋存于锂云母和鳞云母内。铷含量0.1%~0.215%,平均0.133%。铍矿石具细脉状,矿石矿物为细粒状绿柱石,BeO含量0.1%~0.43%,平均0.172%。铌钽矿物为铌铁矿—钽铁矿、细晶石—烧绿石、铌钽金红石类等 大型 白垩纪
Table 1  华北地区典型稀土稀有金属矿床成矿信息
[1] 高凤平, 张璞, 刘大成, 等. 国际稀土市场新格局与中国稀土产业战略选择[J]. 国际贸易问题, 2019(7):63-81.
[1] Gao F P, Zhang P, Liu D C, et al. The rare earths global market updates and the rare earths industry master plan of the united states and its allies[J]. Journal of International Trade, 2019(7):63-81.
[2] 王登红, 王瑞江, 孙艳, 等. 中国三稀矿产资源调查研究成果综述[J]. 地球学报, 2016,37(5):569-580.
[2] Wang D H, Wang R J, Sun Y, et al. A review of achievements in the three-type rare mineral resources (rare resources, rare earth and rarely scattered resources) survey in China[J]. Acta Geoscientica Sinica, 2016,37(5):569-580.
[3] 王登红. 关键矿产的研究意义、矿种厘定、资源属性、找矿进展、存在问题及主攻方向[J]. 地质学报, 2019,93(6):1189-1209.
[3] Wang D H. Study on critical mineral resources: Significance of research, determination of types, attributes of resources, progress of prospecting, problems of utilization, and direction of exploitation[J]. Acta Geological Sinica, 2019,93(6):1189-1209.
[4] 王登红. 战略性关键矿产相关问题探讨[J]. 化工矿产地质, 2019,41(2):65-72.
[4] Wang D H. Discussion on issues related to strategic key mineral resources[J]. Geology of Chemical Minerals, 2019,41(2):65-72.
[5] 范宏瑞, 胡芳芳, 陈福坤, 等. 白云鄂博超大型REE-Nb-Fe矿区碳酸岩墙的侵位年龄——兼答Le Bas博士的质疑[J]. 岩石学报, 2006,22(2):519-520.
[5] Fan H R, Hu F F, Chen F K, et al. Intrusive age of No.1 carbonatite dyke from Bayan Obo REE-Nb-Fe deposit, Inner Mongolia: With answers to comment of Dr.Le Bas[J]. Acta Petrologica Sinica, 2006,22(2):519-520.
[6] 李健康, 袁忠信, 白鸽, 等. 山东微山稀土矿床成矿流体的演化及对成矿的制约[J]. 矿物岩石, 2009,29(3):60-68.
[6] Li J K, Yuan Z X, Bai G, et al. REE-form ing fluid evolvem nt and its controlling to REE (AG) mineralizing in the Weishan deposit, Shandong[J]. Journal of Mineralogy and Petrology, 2009,29(3):60-68.
[7] 刘健, 凌明星, 李印, 等. 白云鄂博超大型REE-Nb-Fe矿床的稀土成矿模式综述[J]. 大地构造与成矿学, 2009,33(2):270-28.
[7] Liu J, Ling M X, Li Y, et al. REE ore-forming models of giant Bayan Obo REE-Nb-Fe ore deposit: A review[J]. Geotectonica et Metallogenia, 2009,33(2):270-28.
[8] 于学峰, 唐好生, 韩作振, 等. 山东郗山—龙宝山地区与碱性岩有关的稀土矿床地质特征及成因[J]. 地质学报, 2010,84(3):407-417.
[8] Yu X F, Tang H S, Han Z Z, et al. Geological characteristics and origin of rare earth elements deposits related with alkaline rock in the Chishan’ Longbaoshan area, Shandong Province[J]. Acta Geologica Sinica, 2010,84(3):407-417.
[9] 李六权, 安林, 上官中江. 小秦岭某地硷性火山岩型稀有、稀土矿化特征及资源潜力[J]. 陕西地质, 2017,35(2):1-6.
[9] Li L Q, An L, Shangguan Z J. Mineralization characteristics,resource potential and prospecting significance of rare and rare earth minerals in alkaline volcanic rocks in small qinling mountains[J]. Geology of Shaanxi, 2017,35(2):1-6.
[10] 章雨旭, 江少卿, 张绮玲, 等. 论内蒙古白云鄂博群和白云鄂博超大型稀土—铌—铁矿床成矿的年代[J]. 中国地质, 2008,35(6):1129-1137.
[10] Zhang Y X, Jiang S Q, Zhang Q L, et al. A discussion on forming time of the Bayan Obo group and ore-forming time of the Bayan Obo giant REE-Nb-Fe deposit,Inner Mongolia[J]. Geology in China, 2008,35(6):1129-1137.
[11] 杜青松, 赵力颖, 李志华, 等. 内蒙古中部花岗岩型稀有金属矿床特征与找矿标志[J]. 中国钼业, 2018,42(2):8-14.
[11] Du Q S, Zhao L Y, Li Z H, et al. Ore characteristics and prospecting marks of granite type rare metal deposits in the middle of the Inner Mongolia autonomous region[J]. China Molybdenum Industy, 2018,42(2):8-14.
[12] 郝美珍, 赵永岗, 张顺, 等. 白云鄂博超大型Nb-Fe-REE矿床主矿矿体形态变化及深部找矿方向的探讨[J]. 地质调查与研究, 2018,41(3):167-175.
[12] Hao M Z, Zhao Y G, Zhang S, et al. Study on the variation of the main ore body form and deep prospecting direction of the giant Bayan Obo Nb-Fe-REE iron ore deposit[J]. Geological Survey and Research, 2018,41(3):167-175.
[13] 费晓杰, 曾普胜, 颜春军, 等. 从同位素年龄看白云鄂博稀土-铌-铁矿床区域地质演化历史[J]. 地质与勘探, 2019,55(2):461-471.
[13] Fei X J, Zeng P S, Yan C J, et al. The regional geological evolution history of the Bayan Obo REE-Nb-Fe deposit derived from isotopic ages[J]. Geology and Exploration, 2019,55(2):461-471.
[14] 徐颖, 孟万涛. 河北省稀有、稀土矿床类型分析[J]. 矿产勘查, 2019,10(2):249-252.
[14] Xu Y, Meng W T. Types of rare and rare earth deposits in Hebei[J]. Mineral Exploration, 2019,10(2):249-252.
[15] 田京祥, 张日田, 范跃春, 等. 山东郗山碱性杂岩体地质特征及与稀土矿的关系[J]. 山东地质, 2002,18(1):21-25.
[15] Tian J X, Zhang R T, Fan Y C, et al. Geological characteristics and relation with rare earth elements of alkalic complex in Chishan of Shandong Province[J]. Geology of Shandong, 2002,18(1):21-25.
[16] 范宏瑞, 胡芳芳, 杨奎锋, 等. 白云鄂博超大型稀土—铌—铁矿床成矿过程中的流体不混溶作用[J]. 矿床地质, 2006,25(S):163-166.
[16] Fan H R, Hu F F, Yang K F, et al. Fluid unmixing/immiscibility as an ore-forming process in the super large REE-Nb-Fe deposit, Inner Mongolian, China[J]. Mineral Deposits, 2006,25(S):163-166.
[17] 朱京占, 张国辉, 杜青松, 等. “八〇一”稀有稀土矿床碱性花岗岩的含矿性、矿化规律及成因分析[J]. 西北地质, 2013,46(4):207-214.
[17] Zhu J Z, Zhang G H, Du Q S, et al. Ore potentiality,mineralization laws and genesis of alkaline granite in 801 rare ree deposit[J]. Northwestern Geology, 2013,46(4):207-214.
[18] 叶松, 周宝霞, 叶德隆, 等. 稀有金属花岗岩的特征及其成矿作用[J]. 岩石矿物学杂志, 2015,34(5):767-776.
[18] Ye S, Zhou B X, Ye D L, et al. Characteristics of the rare metal granite and its mineralization[J]. Acta Petrologica Et Mineralogica, 2015,34(5):767-776.
[19] 梁雨薇, 赖勇, 胡弘, 等. 山东省微山稀土矿正长岩类锆石U-Pb年代学及地球化学特征研究[J]. 北京大学学报:自然科学版, 2017,53(4):652-666.
[19] Liang Y W, Lai Y, Hu H, et al. Zircon U-Pb ages and geochemical characteristics study of syenite from Weishan REE deposit, Western Shandong[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2017,53(4):652-666.
[20] 吴成斌, 侯广顺, 向世红, 等. 东秦岭鱼池正长岩体岩石地球化学特征及稀有金属元素、稀土元素矿化[J]. 地质科技情报, 2017,36(2):58-64.
[20] Wu C B, Hou G S, Xiang S H, et al. Geochemical charateristics of Yuchi syenites from East Qinling and the rare metal elements, rare earth element mineralization[J]. Geological Science and Technology Information, 2017,36(2):58-64.
[21] 程细音, 祝新友, 邹滔. 大兴安岭中南段与花岗岩相关稀有金属矿地质地球化学标志[C]// 第九届全国成矿理论与找矿方法学术讨论会, 2019.
[21] Cheng X Y, Zhu X Y, Zou T. Geological and geochemical indication of granite-related rare metal deposits in the middle and southern section of the Great Xing’an Mountains[C]// The 9th National Symposium on Metallogenic Theory and Prospecting Methods, 2019.
[22] 李俊建. 华北地区重要矿种区域成矿规律研究成果报告[R]. 天津地质调查中心, 2013.
[22] Li J J. Research results on regional metallogenic regularity of important minerals in North China[R]. Tianjin Center, China Geological Survey, 2013.
[23] 董广莹. 苍山龙宝山地区碱性杂岩体金成矿特征研究[D]. 济南:山东科技大学, 2011.
[23] Dong G Y. Study of gold mineralization features of alkaline complex rock mass in longbaoshan area of cangshan country[D]. Jinan: Shandong University of Science and Technology, 2011.
[24] 张正伟, 朱炳泉, 常向阳, 等. 东秦岭北部富碱侵入岩钕、锶、铅同位素特征及构造意义[J]. 地球化学, 2000,29(5):455-461.
[24] Zhang Z W, Zhu B Q, Chang X Y, et al. Nd, Sr, Pb isotopic geochemistry of the alkali-rich intrusive rocks in East Qinling, central China and its tectonic significance[J]. Geochimica, 2000,29(5):455-461.
doi: 10.1016/0016-7037(65)90039-6
[25] 梁涛, 白凤军, 卢欣祥, 等. 河南省方城北部正长岩岩体稀有金属、稀土元素的矿化[J]. 资源导刊:地球科技版, 2014(1):9-12.
[25] Liang T, Bai F J, Lu X X, et al. Mineralization of rare metal elements and rare earth elements in syenite bodies from Northern Fangcheng County, Henan Province[J]. Resources Guide: Earth Science and Technology, 2014(1):9-12.
[26] 王银喜, 李惠民, 杨杰东, 等. 华北古风化壳型稀有稀土矿床的发现及意义[J]. 高校地质学报, 2000,6(4):605-606.
[26] Wang Y X, Li H M, Yang J D. Discovery of Paleoeathering type rare earth deposits in North China and its significance[J]. Geological Journal of China Universities, 2000,6(4):605-606.
[27] 李中明, 赵建敏, 冯辉, 等. 河南省郁山古风化壳型稀土矿层的首次发现及意义[J]. 矿产与地质, 2007,21(2):177-180.
[27] Li Z M, Zhao J M, Feng H, et al. First discovery of palaeo-weathering crust type REE deposit in Yushan area of Henan province and its significance[J]. Mineral Resources and Geology, 2007,21(2):177-180.
[28] 李俊建, 付超, 唐文龙, 等. 内蒙古东乌旗沙麦钨矿床的成矿时代[J]. 地质通报, 2016,35(4):68-74.
[28] Li J J, Fu C, Tang W L, et al. The metallogenic age of the Shamai wolframite deposit in Dong Ujimqin Banner,Inner Mongolia[J]. Geological Bulletin of China, 2016,35(4):524-530.
[29] 王树庆, 胡晓佳, 赵华雷. 内蒙古苏左旗洪格尔地区新发现晚石炭世碱性花岗岩[J]. 地质调查与研究, 2019,42(2):81-85.
[29] Wang S Q, Hu X J, Zhao H L. New discovery of Late Carboniferous alkaline granite in Hongger area, Suzuo Banner, Inner Mongolia[J]. Geological Survey and Research, 2019,42(2):81-85.
[30] 李俊建, 付超, 党智财, 等. 蒙古国矿产资源概况[J]. 地质调查与研究, 2020,43(1):19-29.
[30] Li J J, Fu C, Dang Z C, et al. Overview of mineral resources in Mongolia[J]. Geological Survey and Research, 2020,43(1):19-29.
[31] 邢光福, 洪文涛, 张雪辉, 等. 华东地区燕山期花岗质岩浆与成矿作用关系研究[J]. 岩石学报, 2017,33(5):1571-1590.
[31] Xing G F, Hong W T, Zhang X H, et al. Yanshanian granitic magmatisms and their mineralizations in East China[J]. Acta Petrologica Sinic, 2017,33(5):1571-1590.
[32] 周振玲, 李功元, 宋同云, 等. 内蒙古白云鄂博白云石碳酸岩的地质特征及其成因探讨[J]. 地质论评, 1980,26(1):35-44.
[32] Zhou Z L, Li G Y, Song T Y, et al. Geological characteristics and genesis of dolomite carbonate rocks in Bayan Obo, Inner Mongolia[J]. Geological Review, 1980,26(1):35-44.
[33] 杨晓勇. 白云鄂博铁—稀土—铌矿床地质特征及其研究中存在的科学问题——兼论白云鄂博超大型矿床的成因[J]. 地质学报, 2015,89(12):2323-2350.
[33] Yang X Y. Geological characteristics and their scientific problems of the Bayan Obo Fe-REE-Nb deposit: Discussion on the origin of Bayan Obo super-large deposit[J]. Acta Geologica Sinica, 2015,89(12):2323-2350.
[34] Hoefs J. Stable isotope geochemistry[M]. Berlin: Springer, 1997.
[35] 陶克捷, 杨主明, 张培善, 等. 白云鄂博矿区周围火成碳酸岩岩墙地质特征[J]. 地质科学, 1998,33(1):73-83.
[35] Tao K J, Yang Z M, Zhang S P, et al. Systematic geological investigation on carbonatite dykes in Bayan Obo, Inner Mongolia, China[J]. Chinese Journal of Geology, 1998,33(1):73-83.
[36] Yang X M, Yang X Y, Zheng Y F, et al. A rare earth element-rich carbonatite dyke at Bayan Obo,Inner Mongolia, North China[J]. Mineralogy and Petrology, 2003,78:93-110.
doi: 10.1007/s00710-002-0220-5
[37] 孟庆昌, Drew L J. 白云鄂博碳酸岩矿床的成因特征[J]. 地质与勘探, 1981,17(3):11-15.
[37] Meng Q C, Drew L J. Genetic characteristics of the Bayan Obo carbonate deposit[J]. Geology and Exploration, 1981,17(3):11-15.
[38] 倪振平, 田京祥, 王来明, 等. 山东省重要矿产区域成矿规律[M]. 济南: 山东科学技术出版社, 2016.
[38] Ni Z P, Tian J X, Wang LM, et al. Metallogenic regularity of important mineral resources in Shandong Province[M]. Jinan: Shandong Science and Technology Press, 2016.
[39] 王涛, 刘燊, 胡瑞忠, 等. 苏鲁造山带碱性岩的成因研究——主微量元素地球化学证据[J]. 矿物学报, 2010,30(2):194-206.
[39] Wang T, Liu Y, Hu R Z, et al. Petrogenesis of alkaline rocks in the Sulu orogen:Evidence from elemental geochemistry[J]. Acta Mineralogica Sinica, 2010,30(2):194-206.
[40] 翟明国, 孟庆任, 刘建明, 等. 华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨[J]. 地学前缘, 2004,11(3):285-297.
[40] Zhai M G, Meng Q R, Liu J M. Geological features of mesozoic tectonic regime inversion in Eastern North China and implication for geodynamics[J]. Earth Science Frontiers, 2004,11(3):285-297.
[41] 夏庆霖, 高燕, 王小哈. 鲁西龙宝山金矿成矿流体特征与矿床成因模型[J]. 黄金科学技术, 2002,10(3):13-17.
[41] Xia Q L, Gao Y, Wang X H. Characteristics of metallogenic fluid and genesis model of the longbao mountain gold mine in western shandong province[J]. Gold Science & Technololgy, 2002,10(3):13-17.
[42] 刘琰, 陈超, 舒小超, 等. 青藏高原东部碳酸岩—正长岩杂岩体型REE矿床成矿模式——以大陆槽REE矿床为例[J]. 岩石学报, 2017,33(7):1978-2000.
[42] Liu Y, Chen C, Shu X C, et al. The formation model of the carbonatite-syenite complex REE deposit in the east of Tibetan Plateau: A case study of Dalucao REE deposit[J]. Acta Petrologica Sinica, 2017,33(7):1978-2000.
[43] 白鸽, 袁忠信, 丁孝石, 等. 吉林巴尔哲稀有金属碱性花岗岩的成岩成矿作用讨论[C]//中国地质科学院矿床地质研究所文集, 1980.
[43] Bai G, Yuan Z X, Ding X S, et al. Discussion on the diagenesis and mineralization of the rare metal alkaline granite in Balzhe, Jilin[C]//Proceedings of Institute of Mineral Deposits Geology, Chinese Academy of Geological Sciences, 1980.
[44] Richards J P, McCulloch M T, Chappell B W, et al. Sources of metalin the Porgera gold deposit,Papua New Guinea:Evidence from alteration,isotope,and noble metal geochemistry[J]. Geochim.Cosmochim. Acta, 1991,55:565-580.
[45] 内蒙古自治区地质矿产局. 内蒙古自治区岩石地层[M]. 武汉: 中国地质大学出版社, 1996.
[45] Inner Mongolia Autonomous Region Bureau of Geology and Mineral Resources. Petrostratigraphy of Inner Mongolia autonomous region [M]. Wuhan: China University of Geosciences Press, 1996.
[46] 翟明国, 彭澎. 华北克拉通古元古代构造事件[J]. 岩石学报, 2007,23(11):2665-2682.
[46] Zhai M G, Peng P. Paleoproterozoic events in the North China Craton[J]. Acta Petrologica Sinica, 2007,23(11):2665-2682.
[47] 刘超辉, 刘福来. 华北克拉通中元古代裂解事件:以渣尔泰—白云鄂博—化德裂谷带岩浆与沉积作用研究为例[J]. 岩石学报, 2015,31(10):3107-3128.
[47] Liu C H, Liu F L. The Mesoproterozoic rifting in the North China Craton: A case study for magmatism and sedimentation of the Zhaertai-Bayan Obo-Huade rift zone[J]. Acta Petrologica Sinica, 2015,31(10):3107-3128.
[48] 周振玲, 李功元, 宋同云, 等. 内蒙古白云鄂博白云石碳酸岩的地质特征及其成因探讨[J]. 地质论评, 1980,26(1):35-43.
[48] Zhou Z L, Li G Y, Song T Y, et al. Geological characteristics and genesis of dolomite carbonate rocks in Bayan Obo, Inner Mongolia[J]. Geological Review, 1980,26(1):35-43.
[49] 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:D辑, 1998(S2):1-6.
[49] Tu G C. Discussion on some peculiarities of the formation mechanism of the geological setting of the material composition of the unconventional super-large deposits: a preliminary discussion on the unconventional super-large deposits[J]. Science in China:Series D, 1998 (S2):1-6.
[50] 常全明. 华北地台G层铝土矿控矿条件初探[J]. 唐山工程技术学院学报, 1991,13(3):41-46.
[50] Chang Q M. Preliminary study on ore-controlling conditions of bauxite in G bed of North China platform[J]. Rise and Development of Modern Industrial Education in Tangshan, 1991,13(3):41-46.
[51] 赵新福, 李占轲, 赵少瑞, 等. 华北克拉通南缘早白垩世区域大规模岩浆一热液成矿系统[J]. 地球科学, 2019,44(1):52-68.
[51] Zhao X F, Li Z K, Zhao S R. Early cretaceous regional-scale magmatic-hydrothermal metallogenic system at the southern margin of the North China Carton[J]. Earth Science, 2019,44(1):52-68.
[52] 李志丹, 李效广, 崔玉荣, 等. 内蒙古赵井沟铌钽矿床燕山期成矿:来自LA-MC-ICP-MS独居石,锆石U-Pb和黑云母40Ar-39Ar年龄的证据[J]. 地球科学:中国地质大学学报, 2019,44(1):238-251.
[52] Li Z D, Li X G, Cui Y R, et al. Yanshanian mineralization of Zhaojinggou Nb-Ta deposit, Inner Mongolia:Evidences from the Monazite and Zircon LA-MC-ICP-MS U-Pb and biotite 40Ar-39Ar Geochronology[J]. Earth Science:Journal of China University of Geosciences, 2019,44(1):238-251.
[53] 储同庆. 山东碳酸岩磷灰石的特征及其研究意义[J]. 矿物岩石, 1992,12(3):5-12.
[53] Chu T Q. The characteristics of apatite from carbonatite in shandong and its researching significance[J]. Journal of Mineralogy and Petrology, 1992,12(3):5-12.
[54] 张敏, 袁忠信. 内蒙“八○一”稀有元素碱性花岗岩氧同位素地球化学[C]// 中国地质科学院矿床地质研究所文集(21), 1988.
[54] Zhang M, Yuan Z X. Oxygen isotope geochemistry of the “801” rare elements alkaline granite in Inner Mongolia[C]// Proceedings of Institute of Mineral Deposits Geology, Chinese Academy of Geological Sciences(21), 1988.
[55] 天津地质调查中心. 阴山成矿带小狐狸山和雅布赖地区地质矿产调查成果报告[R]. 天津地质调查中心, 2018.
[55] Tianjin Geological Survey Center. Research result on geological and mineral investigation in Xiaolongshan and Yabulai areas of Yinshan metallogenic belt [R]. Tianjin Center, China Geological Survey, 2018.
[56] 周建波, 郑永飞, 吴元保. 苏鲁造山带西北缘五莲花岗岩中锆石U-Pb年龄及其地质意义[J]. 科学通报, 2002,47(22):67-72.
[56] Zhou J B, Zheng Y F, Wu Y B. Zircon U-Pb ages of Wulian granites in the northwestern margin of the Sulu orogenic belt and their geological significance[J]. Chinese Science Bulletin, 2002,47(22):67-72.
[57] 李俊建, 何玉良, 张彦启, 等. 豫西成矿带成矿区划研究进展[J]. 矿床地质, 2014,33(S1):803-804.
[57] Li J J, He Y L, Zhang Y Q, et al. Research progress of metallogenic regionalization in western Henan metallogenic belt[J]. Mineral Deposits, 2014,33(S1):803-804.
[58] 李俊建, 党智财, 付超, 等. 华北陆块晋冀Al-Fe-Au-Pb-Zn-Ag-Cu-煤成矿带主要地质成矿特征及潜力分析[J]. 地质学报, 2016,90(7):1482-1503.
[58] Li J J, Dang Z C, Fu C, et al. Geological characteristics and mineral resource potential of the Jin-Ji Al-Fe-Au-Pb-Zn-Ag-Cu-coal metallogenic belt in the North China Block[J]. Acta Geologica Sinica, 2016,90(7):1482-1503.
[59] 刘东盛, 周建, 严桃桃, 等. 腾冲地块稀土地球化学背景与泥岩中稀土超常富集特征[J]. 地球学报, 2020,41(6):759-769.
[59] Liu D S, Zhou J, Yan T T, et al. Geochemical background of REEs: Super-enrichment in argillaceous rocks in Tengchong Block[J]. Acta Geoscientica Sinica, 2020,41(6):759-769.
[60] 唐坤, 王学求, 迟清华, 等. 兴蒙-华北地球化学走廊带稀土元素含量与空间分布[J]. 地球科学, 2018,43(3):655-671.
[60] Tang K, Wang X Q, Chi Q H, et al. Concentration and spatial distribution of REE in geochemical transect of Xingmeng orogenic belt, North China Craton[J]. Earth Science, 2018,43(3):655-671.
[61] 王学求, 周建, 迟清华, 等. 中国稀土元素地球化学背景与远景区优选[J]. 地球学报, 2020,41(6):747-758.
[61] Wang X Q, Zhou J, Chi Q H, et al. Geochemical background and distribution of rare earth elements in China: Implications for potential prospects[J]. Acta Geoscientica Sinica, 2020,41(6):747-758.
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