华北克拉通中元古代岩浆事件群与成矿作用
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摘要
华北克拉通在经历了早前寒武纪复杂的多阶段性的构造演化之后，从1.80Ga开始进入一个相对稳定的沉积盖层发育的阶段。接受了巨量的中新元古代的沉积，伴随着沉积作用的同时，形成了与哥伦比亚超大陆裂解有关的一系列热-构造事件群。华北克拉通是全球中元古代时期（1.80~1.00Ga）热-构造事件群最发育的克拉通之一。
华北克拉通中元古代裂解事件群从自老到新可分为5个峰期：峰期Ⅰ发生在1.80~1.77Ga之间，以熊耳群火山岩和五台山、恒山地区的基性岩墙群为代表；峰期Ⅱ发生于约1.72~1.67Ga左右，以所谓AMCG组合（Anorthosite, Mangerite,Charnockite, rapakivi Granite）占统治地位，包括大庙斜长岩、密云-环斑花岗岩、赤城环斑花岗岩、蓝营正长岩、古北口碱性花岗岩、涝洼二长花岗岩、石英二长岩、建平地区辉长岩、闪长岩、二长岩、石英正长岩、紫苏花岗岩，固阳石英正长岩等；峰期Ⅲ发生于约1.63~1.62Ga，以大红峪富钾火山岩、华北南缘龙王□碱性花岗岩和鲁西泰山基性岩墙群为代表。峰期Ⅳ发生于约1.33~1.30Ga期间，以侵入到下马岭组、雾迷山组的基性岩墙（床）和商都、化德、康保地区的花岗岩、二长花岗岩、白云鄂博火成碳酸岩为主。峰期Ⅴ发生于约1.23Ga，以华北克拉通东缘的通化辉绿岩墙、建平-青龙基性岩墙、滦南第四系覆盖的隐伏基性岩体以及沂水地区的辉长岩为主。
本文针对1.72~1.67Ga、1.63~1.62Ga、1.33~1.30Ga、约1.23Ga时期的裂解事件群开展具体的研究工作，获得大量的高精度实验测试数据，搭建了华北克拉通中元古代时期裂解事件群精细年代学格架，丰富了华北克拉通中元古代裂解事件群的内涵，建立了华北克拉通中元古代（1.80~1.00Ga）岩浆事件序列。获得涝洼地区二长花岗岩、石英二长岩的锆石LA-ICPMS U-Pb同位素年龄分别为1695±12Ma，1696±12Ma；获得建平地区侵入岩类锆石SHRIMP、MC-LA-ICPMS U-Pb同位素年龄为1692~1714Ma；获得被常州沟组砂砾岩不整合覆盖的花岗斑岩脉锆石LA-MC-ICPMS、SHRIMP U-Pb同位素年龄分别为1673±10Ma，1669±20Ma；获得固阳瓦窑石英正长岩锆石SHRIMPU-Pb同位素年龄为1702±31Ma；获得泰山红门辉绿岩墙斜锆石SIMS、ID-TIMS年龄分别为1632.4±4.2Ma，1621.1±8.8Ma，发现康保地区1335±4Ma二长花岗岩，获得侵入下马岭组基性岩墙斜锆石ID-TIMS年龄为1320±6Ma；在冀东滦南地区获得冀东隐伏基性岩体的SIMS斜锆石Pb-Pb年龄为1228.3±4.0Ma。
结合区域地质特征、地球化学特点、沉积演化序列，讨论了各期裂解事件群的性质及特点，探讨了华北克拉通与中元古代岩浆事件群有关的成矿作用特点，论述了华北克拉通中元古代时期岩浆事件群的大地构造意义。华北克拉通中元古代时期岩浆事件群具有幕式裂解的特点，1.80~1.77Ga，1.72~1.67Ga，1.63~1.62Ga三个时期的的岩浆事件群标志着哥伦比亚超大陆初始裂解的岩浆事件记录，1.33~1.30Ga期间以及1.23Ga的岩浆事件可能代表了哥伦比亚超大陆的晚期裂解事件。大庙钒钛磁铁矿、白云鄂博Fe-REE-Nb矿床成矿作用与中元古代岩浆事件密切相关。
The North China Craton underwent complicate and multistage tectonic evolutionduring early Precambrian period, and then went into a pediocratic time when the thicksedimentary cover developed since1.8Ga. Accompanying with theMid-Mesoproterozoic sedimentation, a series of thermotectonic events related tobreakup of the Columbian supercontinent occurred. The North China Craton almostbecame the most developed area of thermotectonic events during the period of1.80~1.00Ga(Mesoproterozoic).
Mesoproterozoic breakup events in the North China Craton can be included intofive peak periods in ascending order: PeakⅠoccurred during1.80~1.77Ga and wasrepresented by Xionger volcanic and mafic dyke swarms in Wutai mountain andHengshan area; PeakⅡ followed during1.72~1.67Ga and was dominated by AMCGassemblage, including Damiao anorthosite,Miyun rapakivi granites,Chicheng rapakivigranites,Lanying syenite, Gubeikou alkali granite, Laowa monzogranite and quartzmonzonite, Jianping gabbro,diorite,monzonite, quartz syenite and charnockite,andGuyang quartz syenite et al.; Peak Ⅲ occurred during1.63~1.62Ga, such asDahongyu K-rich volcanic, Longwangzhuang alkaline granite in the southern marginof the North China and gabbro-diabase dykes in the Mount Tai of the westernShandong Province; Peak Ⅳ was during the time of1.33~1.30Ga,for example, maficdykes(sills) which intruded into Xiamaling Formation and Wumishan Formation,(monzonitic) granite in the area of Shangdu,Huade and Kangbao, and Bayan Obobeforsite; Peak Ⅴ happened at about1.23Ga, and buried mafic dyke in EasternHebei Province was typical.
In this paper, further research on the breakup events of1.72~1.67Ga,1.63~1.62Ga,1.33~1.30Ga and about1.23Ga period are introduced.On the base of high precision date from experiment, accurate chronologicalframework of Mesoproterozoic breakup events in the North China Craton is builded,which deepens our cognition on the events, and conduces to build the magmatic events sequence this time. Dates will be introduced in detail as following: zirconLA-ICPMS U-Pb isotopic ages of Laowa monzogranite and quartz monzonite are1695±12Ma and1696±12Ma respectively; zircon SHRIMP、MC-LA-ICPMSU-Pb isotopic age of intrusive rock in Jianping area is1692~1714Ma; zirconLA-MC-ICPMS、SHRIMP U-Pb isotopic ages of granite-prophyry dyke which isunconformably overlain by the conglomerate and sandstone of the ChangzhougouFormation are1673±10Ma and1669±20Ma; zircon SHRIMP U-Pb isotopic age ofGuyang quartz syenite is1702±31Ma; baddeleyite SIMS、ID-TIMS U-Pb isotopicages of the gabbro-diabase dike in the Hongmen scenic region of Mount Tai are1632.4±4.2Ma and1621.1±8.8Ma respectively; age of monzonitic granite fromKangbao area is1335±4Ma, and baddeleyite ID-TIMS U-Pb isotopic age of themafic dyke which intruded into Xiamaling Formation is1320±6Ma; baddeleyiteSIMS Pb-Pb isotopic age of buried mafic dyke in Luannan region of Eastern HebeiProvince is1228.3±4.0Ma.
In reviewing of feature of regional geology and sequence of sedment evolution,in this paper, we discuss the nature and characters of breakup events, the features ofmineralization related to magmatic events in Mesoproterozoic period on the NorthChina Craton and the tectonic significance of these magmatic evens which wereepisodic. The ones of1.80~1.77Ga,1.72~1.67Ga,1.63~1.62Ga are the record ofprimary breakup of the Columbian supercontinent, while other events during1.33~1.30Ga and1.23Ga represent the late period of supercontinent breakup. Themineralization of Damiao vanadic titanomagnetite and Bayan Obo Fe-REE-Nbdeposits are closely correlated to Mesoproterozoic magmatic evens.
华北克拉通中元古代裂解事件群从自老到新可分为5个峰期：峰期Ⅰ发生在1.80~1.77Ga之间，以熊耳群火山岩和五台山、恒山地区的基性岩墙群为代表；峰期Ⅱ发生于约1.72~1.67Ga左右，以所谓AMCG组合（Anorthosite, Mangerite,Charnockite, rapakivi Granite）占统治地位，包括大庙斜长岩、密云-环斑花岗岩、赤城环斑花岗岩、蓝营正长岩、古北口碱性花岗岩、涝洼二长花岗岩、石英二长岩、建平地区辉长岩、闪长岩、二长岩、石英正长岩、紫苏花岗岩，固阳石英正长岩等；峰期Ⅲ发生于约1.63~1.62Ga，以大红峪富钾火山岩、华北南缘龙王□碱性花岗岩和鲁西泰山基性岩墙群为代表。峰期Ⅳ发生于约1.33~1.30Ga期间，以侵入到下马岭组、雾迷山组的基性岩墙（床）和商都、化德、康保地区的花岗岩、二长花岗岩、白云鄂博火成碳酸岩为主。峰期Ⅴ发生于约1.23Ga，以华北克拉通东缘的通化辉绿岩墙、建平-青龙基性岩墙、滦南第四系覆盖的隐伏基性岩体以及沂水地区的辉长岩为主。
本文针对1.72~1.67Ga、1.63~1.62Ga、1.33~1.30Ga、约1.23Ga时期的裂解事件群开展具体的研究工作，获得大量的高精度实验测试数据，搭建了华北克拉通中元古代时期裂解事件群精细年代学格架，丰富了华北克拉通中元古代裂解事件群的内涵，建立了华北克拉通中元古代（1.80~1.00Ga）岩浆事件序列。获得涝洼地区二长花岗岩、石英二长岩的锆石LA-ICPMS U-Pb同位素年龄分别为1695±12Ma，1696±12Ma；获得建平地区侵入岩类锆石SHRIMP、MC-LA-ICPMS U-Pb同位素年龄为1692~1714Ma；获得被常州沟组砂砾岩不整合覆盖的花岗斑岩脉锆石LA-MC-ICPMS、SHRIMP U-Pb同位素年龄分别为1673±10Ma，1669±20Ma；获得固阳瓦窑石英正长岩锆石SHRIMPU-Pb同位素年龄为1702±31Ma；获得泰山红门辉绿岩墙斜锆石SIMS、ID-TIMS年龄分别为1632.4±4.2Ma，1621.1±8.8Ma，发现康保地区1335±4Ma二长花岗岩，获得侵入下马岭组基性岩墙斜锆石ID-TIMS年龄为1320±6Ma；在冀东滦南地区获得冀东隐伏基性岩体的SIMS斜锆石Pb-Pb年龄为1228.3±4.0Ma。
结合区域地质特征、地球化学特点、沉积演化序列，讨论了各期裂解事件群的性质及特点，探讨了华北克拉通与中元古代岩浆事件群有关的成矿作用特点，论述了华北克拉通中元古代时期岩浆事件群的大地构造意义。华北克拉通中元古代时期岩浆事件群具有幕式裂解的特点，1.80~1.77Ga，1.72~1.67Ga，1.63~1.62Ga三个时期的的岩浆事件群标志着哥伦比亚超大陆初始裂解的岩浆事件记录，1.33~1.30Ga期间以及1.23Ga的岩浆事件可能代表了哥伦比亚超大陆的晚期裂解事件。大庙钒钛磁铁矿、白云鄂博Fe-REE-Nb矿床成矿作用与中元古代岩浆事件密切相关。
The North China Craton underwent complicate and multistage tectonic evolutionduring early Precambrian period, and then went into a pediocratic time when the thicksedimentary cover developed since1.8Ga. Accompanying with theMid-Mesoproterozoic sedimentation, a series of thermotectonic events related tobreakup of the Columbian supercontinent occurred. The North China Craton almostbecame the most developed area of thermotectonic events during the period of1.80~1.00Ga(Mesoproterozoic).
Mesoproterozoic breakup events in the North China Craton can be included intofive peak periods in ascending order: PeakⅠoccurred during1.80~1.77Ga and wasrepresented by Xionger volcanic and mafic dyke swarms in Wutai mountain andHengshan area; PeakⅡ followed during1.72~1.67Ga and was dominated by AMCGassemblage, including Damiao anorthosite,Miyun rapakivi granites,Chicheng rapakivigranites,Lanying syenite, Gubeikou alkali granite, Laowa monzogranite and quartzmonzonite, Jianping gabbro,diorite,monzonite, quartz syenite and charnockite,andGuyang quartz syenite et al.; Peak Ⅲ occurred during1.63~1.62Ga, such asDahongyu K-rich volcanic, Longwangzhuang alkaline granite in the southern marginof the North China and gabbro-diabase dykes in the Mount Tai of the westernShandong Province; Peak Ⅳ was during the time of1.33~1.30Ga,for example, maficdykes(sills) which intruded into Xiamaling Formation and Wumishan Formation,(monzonitic) granite in the area of Shangdu,Huade and Kangbao, and Bayan Obobeforsite; Peak Ⅴ happened at about1.23Ga, and buried mafic dyke in EasternHebei Province was typical.
In this paper, further research on the breakup events of1.72~1.67Ga,1.63~1.62Ga,1.33~1.30Ga and about1.23Ga period are introduced.On the base of high precision date from experiment, accurate chronologicalframework of Mesoproterozoic breakup events in the North China Craton is builded,which deepens our cognition on the events, and conduces to build the magmatic events sequence this time. Dates will be introduced in detail as following: zirconLA-ICPMS U-Pb isotopic ages of Laowa monzogranite and quartz monzonite are1695±12Ma and1696±12Ma respectively; zircon SHRIMP、MC-LA-ICPMSU-Pb isotopic age of intrusive rock in Jianping area is1692~1714Ma; zirconLA-MC-ICPMS、SHRIMP U-Pb isotopic ages of granite-prophyry dyke which isunconformably overlain by the conglomerate and sandstone of the ChangzhougouFormation are1673±10Ma and1669±20Ma; zircon SHRIMP U-Pb isotopic age ofGuyang quartz syenite is1702±31Ma; baddeleyite SIMS、ID-TIMS U-Pb isotopicages of the gabbro-diabase dike in the Hongmen scenic region of Mount Tai are1632.4±4.2Ma and1621.1±8.8Ma respectively; age of monzonitic granite fromKangbao area is1335±4Ma, and baddeleyite ID-TIMS U-Pb isotopic age of themafic dyke which intruded into Xiamaling Formation is1320±6Ma; baddeleyiteSIMS Pb-Pb isotopic age of buried mafic dyke in Luannan region of Eastern HebeiProvince is1228.3±4.0Ma.
In reviewing of feature of regional geology and sequence of sedment evolution,in this paper, we discuss the nature and characters of breakup events, the features ofmineralization related to magmatic events in Mesoproterozoic period on the NorthChina Craton and the tectonic significance of these magmatic evens which wereepisodic. The ones of1.80~1.77Ga,1.72~1.67Ga,1.63~1.62Ga are the record ofprimary breakup of the Columbian supercontinent, while other events during1.33~1.30Ga and1.23Ga represent the late period of supercontinent breakup. Themineralization of Damiao vanadic titanomagnetite and Bayan Obo Fe-REE-Nbdeposits are closely correlated to Mesoproterozoic magmatic evens.
引文
2华北克拉通与南非卡普瓦尔克拉通砾岩型金矿铀矿对比研究报告，2012
Andersen T. Correction of common lead in U–Pb analyses that do not report204Pb. Chemicalgeology,2002.192(1):59~79
Chu NC, Taylor RN, Chavagnac V, et al. Hf isotope ratio analysis using multi-collectorinductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections.J. Anal. At. Spectrom,2002.17:1567~1574
Condie KC, Kr ner A. When did plate tectonics begin? Evidence from the geologic record.Geological Society of America Special Paper,2008.440:281~294
Condie KC. Precambrian superplume event. In: Eriksson P G, Altermann W, Nelson DR,Mueller WU, Catuneanu O (Eds.). The Precambrian Earth Tempos and Events: Development inPrecambrian Geology. Amsterdam: Elsevier,2004.163~172
Conrad JE, Mckee EH.40Ar/39Ar dating of vein amphibole from the Bayan Obo iron-rareearth element-niobium deposit, Inner Mongolia, China; constraints on mineralization anddeposition of the Bayan Obo Group. Economic Geology,1992.87(1):185-188
Cui ML, Zhang BL, Zhang LC. U–Pb dating of baddeleyite and zircon from the Shizhaigoudiorite in the southern margin of North China craton: Constrains on the timing and tectonic settingof the Paleoproterozoic Xiong'er group. Gondwana Research,2011.20:184~193
Ernst RE, Wingate MTD, Buchan KL, et al. Global record of1600–700Ma Large IgneousProvinces (LIPs): Implications for the reconstruction of the proposed Nuna (Columbia) andRodinia supercontinents. Precambrian Research,2008.160:159~178
Halls H C, Campal N, Davis DW, et al. Magnetic studies and U-Pb geochronology of theUruguayan dyke swarm, Rio de la Plata craton, Uruguay: Paleomagnetic and economicimplications. Journal of South American Earth Sciences,2001.14:349~361
He YH, Zhao GC, Sun M,, et al. SHRIMP and LA-ICP-MS zircon geochronology of theXiong'er volcanic rocks: implications for the Paleo-Mesoproterozoic evolution of the southernmargin of the North China Craton. Precambrian Research,2009.168(3-4):213~222
He YH, Zhao GC, Sun M. Geochemical and isotopic study of the Xiong’er volcanic rocks atthe southern margin of the North China Craton: Petrogenesis and tectonic implications. the Journalof Geology,2010.118(4):417~433
Hou GT, Li JH, Yang MH, et al. Geochemical constraints on the tectonic environment of thelate Paleoproterozoic mafic dyke swarms in the North China craton. Gondwana Research,2008a.13:103~116
Hou GT, Santosh M, Qian XL, et al. Configuration of the Late Paleoproterozoicsupercontinent Columbia: Insights from radiating mafic dyke swarms. Gondwana Research,2008b.14:395~409
Hu B, Zhai MG, Li TS, Li Z, et al. Mesoproterozoic magmatic events in the eastern NorthChina Craton and their tectonic implications: Geochronological evidence from detrital zircons inthe Shandong Peninsula and North Korea. Gondwana Research,2012.22:828~842
Hu ZC, Gao S, Liu YS, et al. Signal enhancement in laser ablation ICP-MS by addition ofnitrogen in the central channel gas. Journal of Analytical Atomic Spectrometry,2008.23:1093~1101
Jahn BM, Ernst WG. Late Archean Sm-Nd isochron age for mafic-ultramafic supracrustalamphibolites from the northeastern Sino-Korean Craton China. Precambrian Research,1990.46:295~306
Jahn BM, Liu DY, Wan YS, et al. Archean crustal evolution of the Jiaodong Peninsula,China, as revealed by zircon SHRIMP geochronology, elemental and Nd-isotope geochemistry.American Journal of Science,2008.308:232~269
Jahn B M, Zhang Z Q. Radiometric ages (Rb-Sr, Sm-Nd, U-Pb) and REE geochemistry ofArchaean granulite gneisses from eastern Hebei Province, China. In: Kr ner A, Hanson G N,Goodwin A M, Eds. Archaean Geochemistry. Berlin: Springer,1984.183~204
Jiang N, Guo J H, Zhai M G. Nature and origin of the Wenquang granite: Implications for theprovenance of Proterozoic A-type granites in the North China craton. Journal of Asia EarthScience,2011.42:76~82
Krogh T. A low Ocontamination met hod for hydrot hermal decomposition of zircon andextraction of U and Pb for isotopicage determinations. Geochim Cosmochim. Acta.1973,37(3):485~494
Le Bas MJ, Kellere J, Kejie T, et al. Carbonatite dykes at bayan Obo, inner Mongolia, China.Mineralogy and Petrology,1992.46(3):195~228
Le Bas MJ, Spiro B, Yang XM. Oxygen, carbon and strontium isotope study of thecarbonatitic dolomite host of the Bayan Obo Fe-Nb-REE deposit, Inner Mongolia, N China[J].Mineralogical Magazine,1997.61(4):531~541
Le Bas MJ, Yang XM, Taylor RN, et al. New evidence from a calcite-dolomitecarbonatitedyke for the magmatic origin of the massive BayanObo ore-bearing dolomite marble, InnerMongolia, China.Mineralogy and Petrology,90(3-4):223~248
Li QL, Chen FK, Guo JH, et al. Zircon ages and Nd–Hf isotopic composition of the ZhaertaiGroup (Inner Mongolia): Evidence for early Proterozoic evolution of the northern North ChinaCraton. Journal of Asian Earth Sciences,2007.30:573~590
Liu DY, Nutman AP, Compston W, et al. Remnants of≥3800Ma crust in the Chinese part ofthe Sino-Korean craton. Geology,1992.20:339~342
Liu DY, Shen QY, Zhang ZQ, et al. Archean crustal evolution in china: U-Pb geochronologyof the Qianxi Complex. Precambrian Research,1990.48:223~244
Liu DY, Wilde SA, Wan YS, et al. New U-Pb and Hf isotopic data confirm Anshan as theoldest preserved segment of the North China Craton. American Journal Science,2008.308:200~231
Liu SW, Santosh M, Wang W, et al. Zircon U–Pb chronology of the Jianping Complex:Implications for the Precambrian crustal evolution history of the northern margin of North ChinaCraton. Gondwana Research,2011.20:48~63
Liu YS, Hu ZC, Zong KQ, et al. Reappraisement and refinement of zircon U-Pb isotope andtrace element analyses byLA-ICP-MS. Chinese Science Bulletin,2010.55(15):1535~1546
Lu SN, Yang CL, Li HK, et al. A Group of Rifting Events in the Terminal Paleoproterozoicin the North China Craton. Gondwana Research,2002.5(1):123~131
Lu SN, Zhao GC, Wang HC, et al. Precambrian metamorphic basement and sedimentarycover of the North China Craton: A review. Precambrian Research,2008.160:77~93
Ludwig KR. ISOPLOT3.00: A Geochronological Toolkit for Microsoft Excel. BerkeleyGeochronology Center, California, Berkeley,2003.39
Luo Y, Sun M, Zhao GC. LA-ICP-MS U-Pb Zircon Geochronology of the Yushulazi Groupin the Eastern Block, North China Craton. International Geology Review,2006.48:828~840
Meng QR, Wei HH, Qu YQ, Ma SX. Stratigraphic and sedimentary records of the rift to driftevolution of the northern North China craton at the Paleo-to Mesoproterozoic transition.Gondwana Research,2011.20:205~218
Peng P, Liu F, Zhai MG, et al. Age of the Miyun dyke swarm: Constraints on the maximumdepositional age of the Changcheng System. Chinese Science Bulletin,2012.57:105~110
Peng P, Zhai MG, Ernst RE, et al. A1.78Ga large igneous province in the North Chinacraton: The Xiong'er Volcanic Province and the North China dyke swarm. Lithos,2008.101:260~280
Peng P, Zhai M G, Guo J H, et al. Nature of mantle source contributions and crystaldifferentiation in the petrogenesis of the1.78Ga mafic dykes in the central North China craton.Gondwana Research,2007.12:29~46
Peng P, Zhai M G, Zhang H F, et al. Geochronological constraints on the Paleoproterozoicevolution of the North China Craton: SHRIMP zircon ages of different types of mafic dikes.International Geology Review,2005.47:492~508
Peng P. Reconstruction and interpretation of giant mafic dyke swarms: a case study of1.78Ga magmatism in the North China craton. In: Kusky T, Zhai M-G, Xiao W-J, eds. The EvolvingContinents: Understanding Processes of Continental Growth. Geological Society, London, SpecialPublications,2010.338:163~178
Peng P. Zhai M G, Guo J H.1.80-1.75Ga mafic dyke swarms in the central North Chinacraton: implications for a plume-related break-up event. In: Hanski E, Mertanen S, R m T,Vuollo J, eds. Dyke Swarms-Time Markers of Crustal Evolution. London: Taylor&Francis,2006.99~112
Peng, T.P., Wilde, S.A., Fan, W.M, et al. Mesoproterozoic high Fe–Ti mafic magmatisminwestern Shandong, North China Craton: petrogenesis and implications for the final breakup of theColumbia supercontinent. Precambrian Research.2013.235:190~207
Pisarevsky SA, Wingate MTD, Li ZX, et al. Age and paleomagnetism of the1210MaGnowangerup–Fraser dyke swarm, Western Australia, and implications for late Mesoproterozoicpaleogeography.Precambrian Res.2014.246:1~15
R m O T, Haapala I, Vaasjoki M, et al.1700Ma Shachang complex, northeast China:Proterozoic rapakivi granite not associated with Paleoproterozoic orogenic crust. Geology,1995.23(9):815~818
Song B, Nutman A P, Liu D Y, et al.3800to2500Ma crust in the Anshan area of LiaoningProvince, northeastern China. Precambrian Research,1996.78:79~84
Su WB, Zhang SH, Huff WD, et al. SHRIMP U–Pb ages of K-bentonite beds in theXiamaling Formation: Implications for revised subdivision of the Meso-to Neoproterozoic historyof the North China Craton. Gondwana Research,2008.14:543~553
Su WB, Li HK, Huff WD, et al. SHRIMP U-Pb dating for a K-bentonite bed in the TielingFormation, North China. Chinese Science Bulletin,2010.55:3312~3323
Wan YS, Liu DY, Song B, et al. Geochemical and Nd isotopic compositions of3.8Gameta-quartz dioritic and trondhjemitic rocks from the Anshan area and their geologicalsignificance. Journal of Asian Earth Science,2005.24:563~575
Wan YS, Liu DY, Wang W, et al. Provenance of Meso-to Neoproterozoic cover sediments atthe Ming Tombs, Beijing, North China Craton: An integrated study of U–Pb dating and Hfisotopic measurement of detrital zircons and whole-rock geochemistry. Gondwana Research,2011.20:219~242
Wan YS, Liu DY, Nutman A, et al. Multiple3.8–3.1Ga tectono-magmatic events in a newlydiscovered area of ancient rocks (the Shengousi Complex), Anshan, North China Craton [J].Journal of Asian Earth Sciences,2012.54-55:18~30
Wang JW, Tatsumoto M, Li XB, et al. A precise232Th-208Pb chronology of fine-grainedmonazite: Age of the Bayan Obo REE-Fe-Nb ore deposit, China. Geochimica et CosmochimicaActa,1994.58(15):3155~3169
Wang W, Liu SW, Bai X, et al. Geochemistry and zircon U-Pb-Hf isotopes of the latePaleoproterozoic Jianping diorite-monzonite-syenite suite of the North China Craton: Implicationsfor petrogenesis and geodynamic setting. Lithos,2013.175~194
Wang W, Liu SW, Santosh M, et al.1.23Ga mafic dykes in the North China Craton and theirimplications for the reconstruction of the Columbia supercontinent.Gondwana Research,2014.2
Wang W, Liu SW, Santosh M, et al. Late Paleoproterozoic geodynamics of the North ChinaCraton: Geochemical and zircon U-Pb-Hf records from a volcanic suite in the Yanliao rift.Gondwana Research,2013.4
Wang XL, Jiang SY, Dai BZ. Melting of enriched Archean subcontinental lithospheric mantle:Evidence from the ca.1760Ma volcanic rocks of the Xiong’er Group, southern margin of theNorth China Craton. Precambrian Research,2010.182(2010):204~216
Wang XL, Jiang SY, Dai BZ, et al. Lithospheric thinning and reworking of Late Archeanjuvenile crust on the southern margin of the North China Craton: evidence from theLongwangzhuang Paleoproterozoic A-type granites and their surrounding Cretaceous adakite-likegranites. Geological Journal,2013.48(5):498~515
Wang XC, Li ZX, Li J, et al. Genesis of the1.21Ga Marnda Moorn large igneous provinceby plume–lithosphere interaction. Precambrian Res,2014.241:85~103
Wu FY, Zhang YB, Yang JH, et al. Are there any3.8Ga rock at Anshan in the North ChinaCraton?–Reply to comments on “Zircon U–Pb and Hf isotopic constraints on the Early Archeancrustal evolution in Anshan of the North China Craton” by Nutman et al. Precambrian Research,2009.172:361~363
Wu FY, Zhang YB, Yang JH, et al. Zircon U-Pb and Hf isotopic constraints on the EarlyArchean crustal evolution in Anshan of the North China Craton. Precambrian Research,2008.167:339~362
Wu FY, Yang YH, Xie LW, et al. Hf isotopic compositions of the standard zircons andbaddeleyites used in U-Pb geochronology. Chemical Geology,2006.234(1):105~126
Yang KF, Fan HR, Santosh M, et al. Mesoproterozoic mafic and carbonatitic dykes from thenorthern margin of the North China Craton: implications for the final breakup of Columbiasupercontinent. Tectonophysics,2011a.498(1-4):1~10
Yang KF, Fan HR, Santosh M, et al. Mesoproterozoic carbonatitic magmatism in the BayanObo deposit, Inner Mongolia, North China: Constraints for the mechanism of super accumulationof rare earth elements. Ore Geology Reviews,2011b.40(1):122~131
Zhai MG, Bian AG, Zhao TP. The amalgamation of the supercontinent of Noth China Cratonat the end of Neo-Archaean and its breakup during late palaeoproterozoic and Meso-Proterozoic.Science in China (Series D),2000.43:219~232
Zhai MG, Guo JH, Liu W J. Neoarchean to Paleoproterozoic continental evolution andtectonic history of the North China Craton. Journal of Asian Earth sciences,2005.24(5):547~561
Zhai M G, Guo J H, Peng P, et al. U-Pb zircon age dating of a rapakivi granite batholith inRangnim massif, North Korea. Geological magazine,2007.144:547~542
Zhai MG, Li TS, Peng P, et al. Precambrian key tectonic events and evolution of the NorthChina craton. Geological Society, London, Special Publications,2010.338:235~262
Zhai MG, Liu WJ. Palaeoproterozoic tectonic history of the North China craton: A review.Precambrian Research,2003a.122:183~199
Zhai MG, Shao JA, Hao J, et al. Geological signature and possible position of the NorthChina block in the Supercontinent Rodinia. Gondwana Research,2003b.6:171~183
Zhang SH(Shihong), Li ZX, Evans DAD, et al. Pre-Rodinia supercontinent Nuna shaping up:A global synthesis with new paleomagnetic results from North China. Earth and Planetary ScienceLetters,2012b.353-354:145~155
Zhang SH, Liu SW, Zhao Y, et al. The1.75-1.68Ga anorthosite-mangerite-alkaligranitoid-rapakivi granite suite from the northern North China Craton: magmatism related to aPaleoproterozoic orogen. Precambrian Research,2007.155:287~312
Zhang SH, Zhao Y, Santosh M. Mid-Mesoproterozoic bimodal magmatic rocks in thenorthern North China Craton: Implications for magmatism related to breakup of the Columbiasupercontinent. Precambrian Research,2012a.222-223:339~367
Zhang SH, Zhao Y, Yang ZY, et al. The1.35Ga diabase sills from the northern North ChinaCraton: Implications for breakup of the Columbia (Nuna) supercontinent. Earth and PlanetaryScience Letters,2009.288:588~600
Zhao TP, Chen W, Zhou MF. Geochemical and Nd-Hf isotopic constraints on the origin ofthe~1.74Ga Damiao anorthosite complex, North China Craton. Lithos,2009.113(3~4):673~690
Zhao TP, Zhou MF, Zhai MG, et al. Paleoproterozoic rift–related volcanism of the Xiong’ergroup, North China craton: implications for the breakup of Columbia. International GeologyReview,2002.44:336~351
Zhao GC, Cawood PA. Precambrian geology of China. Precambrian Research.2012a.222-223,13~54
Zhao GC, Cawood PA, Wilde SA, et al. Amalgamation of the North China Craton: key issuesand discussion. Precambrian Research.2012b.222-223,55-76
Zhao GC, Sun M, Wilde SA, et al. Assembly, accretion and breakup ofthePaleo-Mesoproterozoic Columbia Supercontinent: records in the North China Craton.Gondwana Research,2003.6:417~434
Zhao GC. Precambrian Evolution of the North China Craton. Elsevier Published,2014
Zhao GC, He YH, Sun M,2009. Xiong’er volcanic belt in the North China Craton:implications for the outward accretion of the Paleo-Mesoproterozoic Columbia (Nuna)Supercontinent. Gondwana Research.16,170-181
Zhao GC, Li SZ, Sun M, Wilde SA,2011a. Assembly, accretion, and break-up of thePalaeo-Mesoproterozoic Columbia supercontinent: records in the North China Craton revisited.International Geology Review.53,1331-1356
Zhao GC, Sun M, Wilde SA, et al. A Paleo-Mesoproterozoic supercontinent: assembly,growth and breakup. Earth Sci. Rev.2004.67:91~123
Zhao GC, Sun M, Wilde SA, et al. Late Archean to Paleoproterozoic evolution of the NorthChina Craton: key issues revisited. Precambrian Research.2005.136:177-202
Zhao GC, Wilde SA, Sun M, et al. SHRIMP U-Pb zircon geochronology of the HuaianComplex: constraints on late Archean to Paleoproterozoic crustal accretion and collision of theTrans-North China Orogen. Am. J. Sci.2008a.308:270~303
Zhao GC, Wilde SA, Sun M, et al. SHRIMP U-Pb zircon ages of granitoid rocks in theLüliang Complex: implications for the accretion and evolution of the Trans-North China Orogen.Precambrian Research.2008b.160:213~226
白鸽,吴澄宇,袁忠信,等.白云鄂博矿床地质特征和成因论证:北京:地质出版社.1996.
白鸽,袁忠信.白云鄂博矿床成因分析.中国地质科学院矿床地质研究所所刊,1983,(4):1~15
白鸽.我对白云鄂博铁铌稀土矿床的研究过程及往见新识.2012,86(5):679~682
包志伟,王强,资锋,等.龙王□A型花岗岩地球化学特征及其地球动力学意义.地球化学,2009,38(6):509~522
曹荣龙,朱寿华,王俊文.白云鄂博铁—稀土矿床的物质来源和成因理论问题.中国科学(B辑),1994,24(12):1298~1307
陈辉,邵济安.白云鄂博地区碳酸岩的形成方式及构造背景//地质矿产部沈阳地质矿产研究所.中国北方板块构造论文集,第2集.北京:地质出版社1987.73~79
陈从云.白云鄂博群渣尔泰群和化德群的时代隶属,中国区域地质,1993,1:59-67
初航,陆松年,王惠初,等.山东长岛地区辅子夼组碎屑锆石年龄谱研究.岩石学报,2011,27(4):1017~1028
刁乃昌.白云鄂博群同位素地质年代学研究,中国区域地质,1990,4:353-359
丁建华,肖成东,秦正永.洞子沟地区大红峪组富钾火山岩岩石学、地球化学特征.地质调查与研究,2005,28(2):100~105
丁悌平,蒋少涌,田世洪,等.白云鄂博矿区赋矿“白云质大理岩”成因的稳定同位素证据.地球学报,2003,24(6):535~542
范宏瑞,陈福坤,王凯怡,等.白云鄂博REE-Fe-Nb矿床酸岩墙锆石U-Pb年龄及其地质意义.岩石学报,2002,18(3):363~368
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.岩石学报,2006,22(2):519~520
范宏瑞,杨奎锋,胡芳芳,等.内蒙古白云鄂博地区基底岩石锆石年代学及对构造背景的指示.岩石学报,2010,26(5):1342~1350
费红彩,肖荣阁,王安建.白云鄂博REE-Nb-Fe稀土矿赋矿岩系建造研究评述.2012,86(5):757~766.
高计元,王一先,裘愉卓,等.白云鄂博矿床含矿白云岩的成因探讨.沉积学报,1999.b17(S1):675~680.
高林志,张传恒,史晓颖,等.华北青白口系下马岭组凝灰岩锆石SHRIMP U-Pb定年.地质通报.2007,26(3):249~255
高林志,张传恒,史晓颖,等.华北古陆下马岭组归属中元古界的SHRIMP锆石新证据.科学通报,2008,53(11):2617~2623
高维,张传恒,高林志,等.北京密云环斑花岗岩的锆石SHRIMP U-Pb年龄及其构造意义.地质通报,2008,27(6):793~798
关保德,耿午辰,戎治权,等.东秦岭北坡震旦亚界.见:王曰伦主编,中国震旦亚界.天津:天津科学技术出版社,1980,288~313
和政军,牛宝贵,张新元,等.2011a.北京密云元古宙常州沟组之下环斑花岗岩古风化壳岩石的发现及其碎屑锆石年龄.地质通报.30(5):798~802
和政军,张新元,牛宝贵,等.北京密云元古宙环斑花岗岩古风化壳及其与长城系常州沟组的关系．地学前缘,2011b.18(4):123~130
洪大卫.密云沙场环斑花岗岩的岩石学研究.北京大学研究生毕业论文，1965
侯贵廷.华北基性岩墙群.北京：科学出版社，2012
侯可军,李延河,邹天人,等. LA-MC-ICPMS锆石Hf同位素的分析方法及地质应用.岩石学报,2007,23(10):2595~2604
侯万荣,肖荣阁,张汉成,等.熊耳裂谷火山岩系金-多金属矿床成矿模式.黄金地质,2003,9:22~27
胡波,翟明国,郭敬辉,等.华北克拉通北缘化德群中碎屑锆石的LA-ICP-MS U-Pb年龄及其构造意义.岩石学报.2009.25(1):193~211
胡波,翟明国,彭澎,等.华北克拉通古元古代末~新元古代地质事件——来自北京西山地区寒武系和侏罗系碎屑锆石LA-ICP-MS U-Pb年代学的证据.岩石学报,2013,29(7):2508~2536
胡俊良,赵太平,徐勇航,等.华北克拉通大红峪组高钾火山岩的地球化学特征及其岩石成因.矿物岩石,2007,27(4):70~77
胡世玲,王松山,桑海清,等.大庙斜长岩同位素地质年龄、稀土地球化学及其地质意义.地质科学,1990,4:332~341
解广轰.大庙斜长岩杂岩体的岩石学特征.地球化学,1980,3:263~280
解广轰,王俊文.大庙斜长岩杂岩体侵位年龄的初步研究.地球化学,1988,1:13-17
解广轰.大庙斜长岩和密云环斑花岗岩的岩石学和地球化学——兼论全球岩体型斜长岩和环斑花岗岩类的时空分布及其意义.北京:科学出版社,2005
李怀坤,李惠民,陆松年.长城系团山子组火山岩颗粒锆石U-Pb年龄及其地质意义.地球化学,1995,24(1):43~48
李怀坤,陆松年,李惠民,等.侵入下马岭组的基性岩床的锆石和斜锆石U-Pb精确定年——对华北中元古界地层划分方案的制约.地质通报,2009,28(10):1396~1404
李怀坤,苏文博,周红英,等.华北克拉通北部长城系底界年龄小于1670Ma——来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMS U-Pb年龄的约束.地学前缘,2011,18(3):108~120
李怀坤,朱士兴,相振群,等.北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束.岩石学报,2010,26(7):2131~2140
李江海,侯贵廷,钱祥麟,等.恒山中元古代早期基性岩墙群的单颗锆石U-Pb年龄及其克拉通构造演化意义.地质论评,2001,47(3):234~238
李云,彭澎,王欣平.华北莱芜地区1680Ma基性岩墙群的特征及其地质意义.2013年全国岩石学与地球动力学研讨会(摘要),2013,136
刘敦一,万渝生,伍家善,等.华北克拉通太古宙地壳演化和最古老的岩石.地质通报,2007,26(9):1131~1138
刘兰笙,高翔,杜安道,等.白云鄂博稀土矿床中辉钼矿的铼-锇同位素年龄.矿床地质,1996,15(2):188~191
刘铁庚,张正伟,叶霖,等.白云鄂博“白云岩”地质地球化学特征及成因讨论,2012,86(5):723~734
刘铁庚.白云鄂博白云岩氧,碳同位素组成及其成因讨论.地质论评,1986,32(2):150~159
刘玉龙,陈江峰,李惠民,等.白云鄂博矿床白云石型矿石中独居石单颗粒U-Th-Pb-Sm-Nd定年.岩石学报,2005a,21(3):881~888
刘玉龙,杨刚,陈江峰,等.白云鄂博超大型稀土-铌-铁矿床黄铁矿Re-Os定年.科学通报,2005b,50(2):172~175
刘玉龙,陈江峰,李惠民,等.白云鄂博矿田碳酸岩墙年代学再研究.地质论评,2006,52(3):415~422
卢冰.大庙斜长岩及其中赋存的黑山铁磷矿床的地球化学.中国科学院广州地球化学研究所博士后出站报告,1995
陆松年,李怀坤,李惠民,等.华北克拉通南缘龙王□碱性花岗岩U-Pb年龄及其地质意义.地质通报,2003,22(10):762~768
陆松年,李惠民.蓟县长城系大红峪组火山岩中锆石精确定年.中国地质科学院院报,1991,22:137~145
陆松年,陈志宏,相振群.泰山世界地质公园古老侵入岩系年代格架.北京:地质出版社,2008,1~90
陆松年,相振群,李怀坤,等.华北克拉通对罗迪尼亚超大陆事件的响应——GOSEN连接假设.地质学报,2012,86(9):1396~1406
陆松年,杨春亮,李怀坤,等.华北古大陆与哥伦比亚超大陆.地学前缘,2002,9(4):225~233
孟庆润, Drew LJ.内蒙白云鄂博“H8含矿白云岩”氧、碳同位素研究及其成因.地质找矿论丛,1992,7(2):46~54
孟庆润.论白云鄂博铁矿含矿围岩——白云岩的沉积成因及其沉积环境分析.地质论评,1982,28(5):481~488
孟宪家,苏振东,包智强,等.白云鄂博群和渣尔泰群的地层和时代对比.中国地质科学院天津地质矿产研究所所刊,1988,20号:32~40
裴福萍,叶轶凡,王枫,等.吉林通化地区中元古代辉绿岩墙的发现及其地质意义.吉林大学学报(地球科学版),2013,43(1):100~108
彭澎,刘富,翟明国,等.密云岩墙群的时代及其对长城系底界年龄的制约.科学通报,2011,56(35):2975~2980
彭澎,翟明国,张华锋,等.华北克拉通1.8Ga镁铁质岩墙群的地球化学特征及其地质意义:以晋冀蒙交界地区为例.岩石学报,2004,20(3):439~456
彭润民,翟裕生,王建平,等.内蒙古狼山新古生代酸性火山岩的发现及其地质意义,科学通报,2010,55(26):2611-2620
彭润民,翟裕生.内蒙古东升庙矿区狼山群中变质“双峰式”火山岩夹层的确认及其意义.地球科学—中国地质大学学报,1997,22(6):589~594
乔秀夫,高林志,彭阳,等.内蒙古腮林忽洞群综合地层和白云鄂博矿床赋矿微晶丘.地质学报,1997,71(3):202-211
乔秀夫,姚培毅,王成述,等.内蒙古渣尔泰群层序地层及构造环境.地质学报,1991,1:1-16
裘愉卓.白云鄂博独居石SHRIMP定年的思考.地球学报,1997,18(S1):211~213
全国地层委员会.中国地层指南及中国地层指南说明书(修订版).北京:地质出版社,2013
任英忱,张英臣,张宗清.白云鄂博稀土超大型矿床的成矿时代及其主要地质热事件.地球学报,1994,15(S1):95~101
邵济安,翟明国,张履桥,等.晋冀蒙交界地区五期岩墙群的界定及其构造意义.地质学报,2005,79(1):56~67
沈保丰,翟安民,陈文明,等.中国前寒武纪成矿作用.北京:地质出版社,2006
宋彪.密云环斑花岗岩的同位素地质年代学、稀土地球化学特征及讨论.中国地质科学院地质研究所所刊,1992,25:137~156
苏文博,李怀坤, Huff WD,等.铁岭组钾质斑脱岩锆石SHRIMP U-Pb年代学研究及其地质意义.科学通报,2010,55(22):2197~2206
苏文博,李怀坤,徐莉,等.华北克拉通南缘洛峪群－汝阳群属于中元古界长城系——河南汝州洛峪口组层凝灰岩锆石LA-MC-ICP MS U-Pb年龄的直接约束.地质调查与研究,2012,35(2):96~108
孙会一,高林志,包创,等.河北宽城中元古代串岭沟组凝灰岩SHRIMP锆石U-Pb年龄及其地质意义.地质学报,2013,87(4):591~596
孙剑,朱祥坤,陈岳龙,等.白云鄂博地区相关地质单元的铁同位素特征及其对白云鄂博矿床成因的制约.2012,86(5):819~828
孙静,杜维河,王德忠,等.河北承德大庙黑山钒钛磁体矿床地质特征与成因探讨.地质学报,2009,83(9):1344~1364
孙枢,张国伟,陈志明.华北断块地区南部前寒武纪地质演化.北京:冶金工业出版社,1985
孙淑芬.内蒙古白云鄂博群尖山组微古植物新发现.地质论评,1992,38(5):474-480
万方晓.北京密云沙厂环斑花岗岩球斑结构的特征及成因探讨.北京地质,1994,3:17~23
万渝生,刘敦一,董春艳,等.中国最老岩石和锆石.岩石学报,2009,25(8):1793~1807
万渝生,刘敦一,殷小艳,等.鞍山地区铁架山花岗岩及表壳岩的锆石SHRIMP年代学和Hf同位素组成.岩石学报,2007,23(02):241~252
万渝生,宋彪,刘敦一,等.鞍山东山风景区3.8~2.5Ga古老岩带的同位素地质年代学和地球化学.地质学报,2001,75(3):363~370
万渝生,张巧大,宋天锐.北京十三陵长城系常州沟组碎屑钻石SHRIMP年龄:华北克拉通盖层物源区及最大沉积年龄的限定.科学通报,2003,48(18):1970~1975
王关玉.河北承德地区斜长岩体的岩石及矿床成矿特征.河北地质情报,1994,4:1-28
王惠初,相振群,赵凤清,等.内蒙古固阳东部碱性侵入岩:年代学、成因与地质意义.岩石学报,2012,28(9):2843~2854
王楫,李双庆,王保良,等.狼山~白云鄂博裂谷系.北京:北京大学出版社,1992
王凯怡,范宏瑞,谢奕汉,等.白云鄂博超大型REE~Fe~Nb矿产基底杂岩的锆石U-Pb年龄.科学通报,2001,46(16):1390~1394
王凯怡,杨奎峰,范宏瑞,等.白云鄂博矿床研究若干问题的探讨,2012,86(5):683~686
魏菊英,蒋少涌,万德芳.内蒙古白云鄂博稀土、铁矿床的硅同位素组成.地球学报,1994,15(1~2):102~110
魏菊英,上官志冠.白云鄂博铁矿围岩白云岩的氧、碳同位素组成及其成因//岩石学研究(第二辑).北京:地质出版社,1983,14~21
吴福元,李献华,郑永飞,等. Lu-Hf同位素体系及其岩石学应用.岩石学报,2007,23(2):185~220
相振群,李怀坤,陆松年,等.泰山地区古元古代末期基性岩墙形成时代厘定——斜锆石U-Pb精确定年.岩石学报,2012,28(9):2831~2842
肖荣阁,费红彩,王安建,等.白云鄂博含矿碱性火山岩建造及其地球化学,2012,86(5):735~752
邢长明,陈伟,王焰,等.华北克拉通北缘元古宙大庙Fe-Ti-P矿床的挥发份组成和C~H~O同位素研究.岩石学报,27(05):1500~1510
徐德斌,白志达,王敦则,等.河北省兴隆地区大红峪组沉积古环境研究.地层学杂志,2002,26(1):73~79
徐平,吴福元,谢烈文,等. U-Pb同位素定年标准锆石的Hf同位素.科学通报,2004.49:1403~1410
阎国翰,郭立鹤,钱彬.承德黑山苏长岩中斜长石研究.北京大学地质系“研究生论文集”,北京:北京大学出版社,1985,106~114
阎国翰,牟保磊.承德黑山斜长杂岩体辉石特征及其形成温度条件.岩石学报,1993,9(3):300~307
杨进辉,吴福元,柳小明,等.北京密云环斑花岗岩锆石U-Pb年龄和Hf同位素及地质意义.岩石学报,2005,21(6):1633~1644
杨奎锋,范宏瑞,胡芳芳,等.白云鄂博陆缘裂谷系沉积物源与超大型稀土矿床含矿白云岩的成因探讨.2012,86(5):775~784
杨岳衡,孙金凤,谢烈文,等.地质样品Nd同位素激光原位等离子体质谱(LA-MC-ICPMS)测定.科学通报,2008.53(5):568~576
郁建华.北京及附近元古宙裂谷槽中球斑花岗岩套的地球化学.地质学报,1990,64(4):322~336
郁建华,付会芹, I.哈巴拉,等.华北克拉通北部1.70Ga非造山环斑花岗岩岩套.华北地质矿产杂志,1996,11(3):9~18
郁建华,付会芹,张凤兰,等.华北地台北部非造山环斑花岗岩及有关岩石.北京:中国科学技术出版社,1996,1~182
袁忠信.再谈白云鄂博矿床的成矿时代和矿床成因.2012,86(5):683~686
翟明国,卞爱国.华北克拉通新太古代末超大陆拼合及古元古代末—中元古代裂解.中国科学(D辑),2000,30:129~137
翟明国,胡波,彭澎,等.华北中~新元古代的岩浆作用与多期裂谷事件.地学前缘,2014,21(1):100~119
翟明国,彭澎.华北克拉通古元古代构造事件.岩石学报,2007,23(11):2665~2682
翟明国.华北克拉通2.1~1.7Ga地质事件群的分解和构造意义探讨.岩石学报,2004.20(6):1343~1354
翟明国.华北克拉通的形成演化与成矿作用.矿床地质,2010,29(1):24~36
翟裕生.某斜长岩的岩石特征及成因.地质论评,1965,23(3):186~195
张汉成,肖荣阁,安国英,等.熊耳群火山岩系金银多金属矿床热水成矿作用.中国地质,2003,34(4):400~405
张华锋,周志广,刘文灿,等.内蒙古中部白乃庙地区格林威尔岩浆事件记录:石英二长闪长岩脉锆石LA-ICP-MS U-Pb年龄证据.岩石学报,2009,25:1512~1518
张鹏远,牛绍武,王长尧,等.白云鄂博地区地质构造特征.中国地质科学院天津地质研究所所刊(第28号).北京:地质出版社,1993,1~86
张拴宏,赵越,叶浩,等.燕辽地区长城系串岭沟组及团山子组沉积时代的新制约.岩石学报.2013,29(07):2481~2490
张维,张福斌,张天龙,等.在第四系覆盖区重磁异常上如何辨别基性岩体与铁矿异常.地质调查与研究,2014
张宗清,唐索寒,王进辉,等.白云鄂博稀土矿床形成年龄的新数据.地球学报,1994,15(1~2):85~94.
张宗清,袁忠信,唐索寒,等.白云鄂博矿床年龄和地球化学.北京:地质出版社,2003
章雨旭,吕洪波,王俊,等.白云鄂博矿床成矿构造环境分析.2012,86(5):767~774
章雨旭,吕洪波,张绮玲,等.微晶丘成因新认识.地球科学进展,2005,20(6):693~700
章雨旭,彭阳,乔秀夫,等.白云鄂博矿床赋矿白云岩成因新认识.地质论评,1998,44(1):70~76.
章雨旭,杨占峰,张绮玲,等.白云鄂博矿床及北京西山微晶丘地质、地球化学研究.北京:地质出版社,2009
赵崇贺.北京密云斜长环斑花岗岩地质学和岩石学研究.第一届矿物岩石地球化学学术会议论文集——岩石部分.北京:科学出版社,1964,124~143
赵太平,陈福坤,翟明国,等.河北大庙斜长岩杂岩体锆石U–Pb年龄及其地质意义.岩石学报.2004b.20(3):685~690
赵太平.华北陆块元古宙熊耳群火山岩、大庙斜长岩杂岩岩体的年代学、岩石地球化学与构造环境研究.中国科学院广州地球化学研究所博士后出站报告,2003
赵太平,金成伟,翟明国,等.华北陆块南部熊耳群火山岩的地球化学特征与成因.岩石学报,2002,18(1):59~69
赵太平,王建平,张忠慧,等.中国王屋山及邻区元古宙地质研究.北京:中国大地出版社,2005
赵太平,徐勇航,翟明国.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议.高校地质学报,2007,13(2):191~206
赵太平,翟明国,夏斌,等.熊耳群火山岩锆石SHRIMP年代学研究:对华北克拉通盖层发育初始时间的制约.科学通报,2004a,49(22):2342~2349
赵太平,周美夫,金成伟,等.华北陆块南缘熊耳群形成时代讨论.地质科学,2001,36(3):326~334
钟富道,解广轰,等.斜长岩事件年龄及其地质意义.地球化学,1978,3:202~208
周建波,郑永飞,杨晓勇,等.白云鄂博地区构造格局与古板块构造演化.高校地质学报,2002,8(1):46~61
周永昶,袁朝.大庙斜长岩杂岩体及铁磷矿的稀土元素地球化学研究.长春地质学院学报,1989,19(1):43~53
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.地质论评,1980,26(1):35~41
朱士兴,邢裕盛,张鹏远.华北地台中、上元古界生物地层序列.北京:地质出版社,1994
朱祥坤,孙剑.内蒙古白云鄂博矿床的稀土矿化时代与期次.地球学报,2012,33(6):845-855
Andersen T. Correction of common lead in U–Pb analyses that do not report204Pb. Chemicalgeology,2002.192(1):59~79
Chu NC, Taylor RN, Chavagnac V, et al. Hf isotope ratio analysis using multi-collectorinductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections.J. Anal. At. Spectrom,2002.17:1567~1574
Condie KC, Kr ner A. When did plate tectonics begin? Evidence from the geologic record.Geological Society of America Special Paper,2008.440:281~294
Condie KC. Precambrian superplume event. In: Eriksson P G, Altermann W, Nelson DR,Mueller WU, Catuneanu O (Eds.). The Precambrian Earth Tempos and Events: Development inPrecambrian Geology. Amsterdam: Elsevier,2004.163~172
Conrad JE, Mckee EH.40Ar/39Ar dating of vein amphibole from the Bayan Obo iron-rareearth element-niobium deposit, Inner Mongolia, China; constraints on mineralization anddeposition of the Bayan Obo Group. Economic Geology,1992.87(1):185-188
Cui ML, Zhang BL, Zhang LC. U–Pb dating of baddeleyite and zircon from the Shizhaigoudiorite in the southern margin of North China craton: Constrains on the timing and tectonic settingof the Paleoproterozoic Xiong'er group. Gondwana Research,2011.20:184~193
Ernst RE, Wingate MTD, Buchan KL, et al. Global record of1600–700Ma Large IgneousProvinces (LIPs): Implications for the reconstruction of the proposed Nuna (Columbia) andRodinia supercontinents. Precambrian Research,2008.160:159~178
Halls H C, Campal N, Davis DW, et al. Magnetic studies and U-Pb geochronology of theUruguayan dyke swarm, Rio de la Plata craton, Uruguay: Paleomagnetic and economicimplications. Journal of South American Earth Sciences,2001.14:349~361
He YH, Zhao GC, Sun M,, et al. SHRIMP and LA-ICP-MS zircon geochronology of theXiong'er volcanic rocks: implications for the Paleo-Mesoproterozoic evolution of the southernmargin of the North China Craton. Precambrian Research,2009.168(3-4):213~222
He YH, Zhao GC, Sun M. Geochemical and isotopic study of the Xiong’er volcanic rocks atthe southern margin of the North China Craton: Petrogenesis and tectonic implications. the Journalof Geology,2010.118(4):417~433
Hou GT, Li JH, Yang MH, et al. Geochemical constraints on the tectonic environment of thelate Paleoproterozoic mafic dyke swarms in the North China craton. Gondwana Research,2008a.13:103~116
Hou GT, Santosh M, Qian XL, et al. Configuration of the Late Paleoproterozoicsupercontinent Columbia: Insights from radiating mafic dyke swarms. Gondwana Research,2008b.14:395~409
Hu B, Zhai MG, Li TS, Li Z, et al. Mesoproterozoic magmatic events in the eastern NorthChina Craton and their tectonic implications: Geochronological evidence from detrital zircons inthe Shandong Peninsula and North Korea. Gondwana Research,2012.22:828~842
Hu ZC, Gao S, Liu YS, et al. Signal enhancement in laser ablation ICP-MS by addition ofnitrogen in the central channel gas. Journal of Analytical Atomic Spectrometry,2008.23:1093~1101
Jahn BM, Ernst WG. Late Archean Sm-Nd isochron age for mafic-ultramafic supracrustalamphibolites from the northeastern Sino-Korean Craton China. Precambrian Research,1990.46:295~306
Jahn BM, Liu DY, Wan YS, et al. Archean crustal evolution of the Jiaodong Peninsula,China, as revealed by zircon SHRIMP geochronology, elemental and Nd-isotope geochemistry.American Journal of Science,2008.308:232~269
Jahn B M, Zhang Z Q. Radiometric ages (Rb-Sr, Sm-Nd, U-Pb) and REE geochemistry ofArchaean granulite gneisses from eastern Hebei Province, China. In: Kr ner A, Hanson G N,Goodwin A M, Eds. Archaean Geochemistry. Berlin: Springer,1984.183~204
Jiang N, Guo J H, Zhai M G. Nature and origin of the Wenquang granite: Implications for theprovenance of Proterozoic A-type granites in the North China craton. Journal of Asia EarthScience,2011.42:76~82
Krogh T. A low Ocontamination met hod for hydrot hermal decomposition of zircon andextraction of U and Pb for isotopicage determinations. Geochim Cosmochim. Acta.1973,37(3):485~494
Le Bas MJ, Kellere J, Kejie T, et al. Carbonatite dykes at bayan Obo, inner Mongolia, China.Mineralogy and Petrology,1992.46(3):195~228
Le Bas MJ, Spiro B, Yang XM. Oxygen, carbon and strontium isotope study of thecarbonatitic dolomite host of the Bayan Obo Fe-Nb-REE deposit, Inner Mongolia, N China[J].Mineralogical Magazine,1997.61(4):531~541
Le Bas MJ, Yang XM, Taylor RN, et al. New evidence from a calcite-dolomitecarbonatitedyke for the magmatic origin of the massive BayanObo ore-bearing dolomite marble, InnerMongolia, China.Mineralogy and Petrology,90(3-4):223~248
Li QL, Chen FK, Guo JH, et al. Zircon ages and Nd–Hf isotopic composition of the ZhaertaiGroup (Inner Mongolia): Evidence for early Proterozoic evolution of the northern North ChinaCraton. Journal of Asian Earth Sciences,2007.30:573~590
Liu DY, Nutman AP, Compston W, et al. Remnants of≥3800Ma crust in the Chinese part ofthe Sino-Korean craton. Geology,1992.20:339~342
Liu DY, Shen QY, Zhang ZQ, et al. Archean crustal evolution in china: U-Pb geochronologyof the Qianxi Complex. Precambrian Research,1990.48:223~244
Liu DY, Wilde SA, Wan YS, et al. New U-Pb and Hf isotopic data confirm Anshan as theoldest preserved segment of the North China Craton. American Journal Science,2008.308:200~231
Liu SW, Santosh M, Wang W, et al. Zircon U–Pb chronology of the Jianping Complex:Implications for the Precambrian crustal evolution history of the northern margin of North ChinaCraton. Gondwana Research,2011.20:48~63
Liu YS, Hu ZC, Zong KQ, et al. Reappraisement and refinement of zircon U-Pb isotope andtrace element analyses byLA-ICP-MS. Chinese Science Bulletin,2010.55(15):1535~1546
Lu SN, Yang CL, Li HK, et al. A Group of Rifting Events in the Terminal Paleoproterozoicin the North China Craton. Gondwana Research,2002.5(1):123~131
Lu SN, Zhao GC, Wang HC, et al. Precambrian metamorphic basement and sedimentarycover of the North China Craton: A review. Precambrian Research,2008.160:77~93
Ludwig KR. ISOPLOT3.00: A Geochronological Toolkit for Microsoft Excel. BerkeleyGeochronology Center, California, Berkeley,2003.39
Luo Y, Sun M, Zhao GC. LA-ICP-MS U-Pb Zircon Geochronology of the Yushulazi Groupin the Eastern Block, North China Craton. International Geology Review,2006.48:828~840
Meng QR, Wei HH, Qu YQ, Ma SX. Stratigraphic and sedimentary records of the rift to driftevolution of the northern North China craton at the Paleo-to Mesoproterozoic transition.Gondwana Research,2011.20:205~218
Peng P, Liu F, Zhai MG, et al. Age of the Miyun dyke swarm: Constraints on the maximumdepositional age of the Changcheng System. Chinese Science Bulletin,2012.57:105~110
Peng P, Zhai MG, Ernst RE, et al. A1.78Ga large igneous province in the North Chinacraton: The Xiong'er Volcanic Province and the North China dyke swarm. Lithos,2008.101:260~280
Peng P, Zhai M G, Guo J H, et al. Nature of mantle source contributions and crystaldifferentiation in the petrogenesis of the1.78Ga mafic dykes in the central North China craton.Gondwana Research,2007.12:29~46
Peng P, Zhai M G, Zhang H F, et al. Geochronological constraints on the Paleoproterozoicevolution of the North China Craton: SHRIMP zircon ages of different types of mafic dikes.International Geology Review,2005.47:492~508
Peng P. Reconstruction and interpretation of giant mafic dyke swarms: a case study of1.78Ga magmatism in the North China craton. In: Kusky T, Zhai M-G, Xiao W-J, eds. The EvolvingContinents: Understanding Processes of Continental Growth. Geological Society, London, SpecialPublications,2010.338:163~178
Peng P. Zhai M G, Guo J H.1.80-1.75Ga mafic dyke swarms in the central North Chinacraton: implications for a plume-related break-up event. In: Hanski E, Mertanen S, R m T,Vuollo J, eds. Dyke Swarms-Time Markers of Crustal Evolution. London: Taylor&Francis,2006.99~112
Peng, T.P., Wilde, S.A., Fan, W.M, et al. Mesoproterozoic high Fe–Ti mafic magmatisminwestern Shandong, North China Craton: petrogenesis and implications for the final breakup of theColumbia supercontinent. Precambrian Research.2013.235:190~207
Pisarevsky SA, Wingate MTD, Li ZX, et al. Age and paleomagnetism of the1210MaGnowangerup–Fraser dyke swarm, Western Australia, and implications for late Mesoproterozoicpaleogeography.Precambrian Res.2014.246:1~15
R m O T, Haapala I, Vaasjoki M, et al.1700Ma Shachang complex, northeast China:Proterozoic rapakivi granite not associated with Paleoproterozoic orogenic crust. Geology,1995.23(9):815~818
Song B, Nutman A P, Liu D Y, et al.3800to2500Ma crust in the Anshan area of LiaoningProvince, northeastern China. Precambrian Research,1996.78:79~84
Su WB, Zhang SH, Huff WD, et al. SHRIMP U–Pb ages of K-bentonite beds in theXiamaling Formation: Implications for revised subdivision of the Meso-to Neoproterozoic historyof the North China Craton. Gondwana Research,2008.14:543~553
Su WB, Li HK, Huff WD, et al. SHRIMP U-Pb dating for a K-bentonite bed in the TielingFormation, North China. Chinese Science Bulletin,2010.55:3312~3323
Wan YS, Liu DY, Song B, et al. Geochemical and Nd isotopic compositions of3.8Gameta-quartz dioritic and trondhjemitic rocks from the Anshan area and their geologicalsignificance. Journal of Asian Earth Science,2005.24:563~575
Wan YS, Liu DY, Wang W, et al. Provenance of Meso-to Neoproterozoic cover sediments atthe Ming Tombs, Beijing, North China Craton: An integrated study of U–Pb dating and Hfisotopic measurement of detrital zircons and whole-rock geochemistry. Gondwana Research,2011.20:219~242
Wan YS, Liu DY, Nutman A, et al. Multiple3.8–3.1Ga tectono-magmatic events in a newlydiscovered area of ancient rocks (the Shengousi Complex), Anshan, North China Craton [J].Journal of Asian Earth Sciences,2012.54-55:18~30
Wang JW, Tatsumoto M, Li XB, et al. A precise232Th-208Pb chronology of fine-grainedmonazite: Age of the Bayan Obo REE-Fe-Nb ore deposit, China. Geochimica et CosmochimicaActa,1994.58(15):3155~3169
Wang W, Liu SW, Bai X, et al. Geochemistry and zircon U-Pb-Hf isotopes of the latePaleoproterozoic Jianping diorite-monzonite-syenite suite of the North China Craton: Implicationsfor petrogenesis and geodynamic setting. Lithos,2013.175~194
Wang W, Liu SW, Santosh M, et al.1.23Ga mafic dykes in the North China Craton and theirimplications for the reconstruction of the Columbia supercontinent.Gondwana Research,2014.2
Wang W, Liu SW, Santosh M, et al. Late Paleoproterozoic geodynamics of the North ChinaCraton: Geochemical and zircon U-Pb-Hf records from a volcanic suite in the Yanliao rift.Gondwana Research,2013.4
Wang XL, Jiang SY, Dai BZ. Melting of enriched Archean subcontinental lithospheric mantle:Evidence from the ca.1760Ma volcanic rocks of the Xiong’er Group, southern margin of theNorth China Craton. Precambrian Research,2010.182(2010):204~216
Wang XL, Jiang SY, Dai BZ, et al. Lithospheric thinning and reworking of Late Archeanjuvenile crust on the southern margin of the North China Craton: evidence from theLongwangzhuang Paleoproterozoic A-type granites and their surrounding Cretaceous adakite-likegranites. Geological Journal,2013.48(5):498~515
Wang XC, Li ZX, Li J, et al. Genesis of the1.21Ga Marnda Moorn large igneous provinceby plume–lithosphere interaction. Precambrian Res,2014.241:85~103
Wu FY, Zhang YB, Yang JH, et al. Are there any3.8Ga rock at Anshan in the North ChinaCraton?–Reply to comments on “Zircon U–Pb and Hf isotopic constraints on the Early Archeancrustal evolution in Anshan of the North China Craton” by Nutman et al. Precambrian Research,2009.172:361~363
Wu FY, Zhang YB, Yang JH, et al. Zircon U-Pb and Hf isotopic constraints on the EarlyArchean crustal evolution in Anshan of the North China Craton. Precambrian Research,2008.167:339~362
Wu FY, Yang YH, Xie LW, et al. Hf isotopic compositions of the standard zircons andbaddeleyites used in U-Pb geochronology. Chemical Geology,2006.234(1):105~126
Yang KF, Fan HR, Santosh M, et al. Mesoproterozoic mafic and carbonatitic dykes from thenorthern margin of the North China Craton: implications for the final breakup of Columbiasupercontinent. Tectonophysics,2011a.498(1-4):1~10
Yang KF, Fan HR, Santosh M, et al. Mesoproterozoic carbonatitic magmatism in the BayanObo deposit, Inner Mongolia, North China: Constraints for the mechanism of super accumulationof rare earth elements. Ore Geology Reviews,2011b.40(1):122~131
Zhai MG, Bian AG, Zhao TP. The amalgamation of the supercontinent of Noth China Cratonat the end of Neo-Archaean and its breakup during late palaeoproterozoic and Meso-Proterozoic.Science in China (Series D),2000.43:219~232
Zhai MG, Guo JH, Liu W J. Neoarchean to Paleoproterozoic continental evolution andtectonic history of the North China Craton. Journal of Asian Earth sciences,2005.24(5):547~561
Zhai M G, Guo J H, Peng P, et al. U-Pb zircon age dating of a rapakivi granite batholith inRangnim massif, North Korea. Geological magazine,2007.144:547~542
Zhai MG, Li TS, Peng P, et al. Precambrian key tectonic events and evolution of the NorthChina craton. Geological Society, London, Special Publications,2010.338:235~262
Zhai MG, Liu WJ. Palaeoproterozoic tectonic history of the North China craton: A review.Precambrian Research,2003a.122:183~199
Zhai MG, Shao JA, Hao J, et al. Geological signature and possible position of the NorthChina block in the Supercontinent Rodinia. Gondwana Research,2003b.6:171~183
Zhang SH(Shihong), Li ZX, Evans DAD, et al. Pre-Rodinia supercontinent Nuna shaping up:A global synthesis with new paleomagnetic results from North China. Earth and Planetary ScienceLetters,2012b.353-354:145~155
Zhang SH, Liu SW, Zhao Y, et al. The1.75-1.68Ga anorthosite-mangerite-alkaligranitoid-rapakivi granite suite from the northern North China Craton: magmatism related to aPaleoproterozoic orogen. Precambrian Research,2007.155:287~312
Zhang SH, Zhao Y, Santosh M. Mid-Mesoproterozoic bimodal magmatic rocks in thenorthern North China Craton: Implications for magmatism related to breakup of the Columbiasupercontinent. Precambrian Research,2012a.222-223:339~367
Zhang SH, Zhao Y, Yang ZY, et al. The1.35Ga diabase sills from the northern North ChinaCraton: Implications for breakup of the Columbia (Nuna) supercontinent. Earth and PlanetaryScience Letters,2009.288:588~600
Zhao TP, Chen W, Zhou MF. Geochemical and Nd-Hf isotopic constraints on the origin ofthe~1.74Ga Damiao anorthosite complex, North China Craton. Lithos,2009.113(3~4):673~690
Zhao TP, Zhou MF, Zhai MG, et al. Paleoproterozoic rift–related volcanism of the Xiong’ergroup, North China craton: implications for the breakup of Columbia. International GeologyReview,2002.44:336~351
Zhao GC, Cawood PA. Precambrian geology of China. Precambrian Research.2012a.222-223,13~54
Zhao GC, Cawood PA, Wilde SA, et al. Amalgamation of the North China Craton: key issuesand discussion. Precambrian Research.2012b.222-223,55-76
Zhao GC, Sun M, Wilde SA, et al. Assembly, accretion and breakup ofthePaleo-Mesoproterozoic Columbia Supercontinent: records in the North China Craton.Gondwana Research,2003.6:417~434
Zhao GC. Precambrian Evolution of the North China Craton. Elsevier Published,2014
Zhao GC, He YH, Sun M,2009. Xiong’er volcanic belt in the North China Craton:implications for the outward accretion of the Paleo-Mesoproterozoic Columbia (Nuna)Supercontinent. Gondwana Research.16,170-181
Zhao GC, Li SZ, Sun M, Wilde SA,2011a. Assembly, accretion, and break-up of thePalaeo-Mesoproterozoic Columbia supercontinent: records in the North China Craton revisited.International Geology Review.53,1331-1356
Zhao GC, Sun M, Wilde SA, et al. A Paleo-Mesoproterozoic supercontinent: assembly,growth and breakup. Earth Sci. Rev.2004.67:91~123
Zhao GC, Sun M, Wilde SA, et al. Late Archean to Paleoproterozoic evolution of the NorthChina Craton: key issues revisited. Precambrian Research.2005.136:177-202
Zhao GC, Wilde SA, Sun M, et al. SHRIMP U-Pb zircon geochronology of the HuaianComplex: constraints on late Archean to Paleoproterozoic crustal accretion and collision of theTrans-North China Orogen. Am. J. Sci.2008a.308:270~303
Zhao GC, Wilde SA, Sun M, et al. SHRIMP U-Pb zircon ages of granitoid rocks in theLüliang Complex: implications for the accretion and evolution of the Trans-North China Orogen.Precambrian Research.2008b.160:213~226
白鸽,吴澄宇,袁忠信,等.白云鄂博矿床地质特征和成因论证:北京:地质出版社.1996.
白鸽,袁忠信.白云鄂博矿床成因分析.中国地质科学院矿床地质研究所所刊,1983,(4):1~15
白鸽.我对白云鄂博铁铌稀土矿床的研究过程及往见新识.2012,86(5):679~682
包志伟,王强,资锋,等.龙王□A型花岗岩地球化学特征及其地球动力学意义.地球化学,2009,38(6):509~522
曹荣龙,朱寿华,王俊文.白云鄂博铁—稀土矿床的物质来源和成因理论问题.中国科学(B辑),1994,24(12):1298~1307
陈辉,邵济安.白云鄂博地区碳酸岩的形成方式及构造背景//地质矿产部沈阳地质矿产研究所.中国北方板块构造论文集,第2集.北京:地质出版社1987.73~79
陈从云.白云鄂博群渣尔泰群和化德群的时代隶属,中国区域地质,1993,1:59-67
初航,陆松年,王惠初,等.山东长岛地区辅子夼组碎屑锆石年龄谱研究.岩石学报,2011,27(4):1017~1028
刁乃昌.白云鄂博群同位素地质年代学研究,中国区域地质,1990,4:353-359
丁建华,肖成东,秦正永.洞子沟地区大红峪组富钾火山岩岩石学、地球化学特征.地质调查与研究,2005,28(2):100~105
丁悌平,蒋少涌,田世洪,等.白云鄂博矿区赋矿“白云质大理岩”成因的稳定同位素证据.地球学报,2003,24(6):535~542
范宏瑞,陈福坤,王凯怡,等.白云鄂博REE-Fe-Nb矿床酸岩墙锆石U-Pb年龄及其地质意义.岩石学报,2002,18(3):363~368
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.岩石学报,2006,22(2):519~520
范宏瑞,杨奎锋,胡芳芳,等.内蒙古白云鄂博地区基底岩石锆石年代学及对构造背景的指示.岩石学报,2010,26(5):1342~1350
费红彩,肖荣阁,王安建.白云鄂博REE-Nb-Fe稀土矿赋矿岩系建造研究评述.2012,86(5):757~766.
高计元,王一先,裘愉卓,等.白云鄂博矿床含矿白云岩的成因探讨.沉积学报,1999.b17(S1):675~680.
高林志,张传恒,史晓颖,等.华北青白口系下马岭组凝灰岩锆石SHRIMP U-Pb定年.地质通报.2007,26(3):249~255
高林志,张传恒,史晓颖,等.华北古陆下马岭组归属中元古界的SHRIMP锆石新证据.科学通报,2008,53(11):2617~2623
高维,张传恒,高林志,等.北京密云环斑花岗岩的锆石SHRIMP U-Pb年龄及其构造意义.地质通报,2008,27(6):793~798
关保德,耿午辰,戎治权,等.东秦岭北坡震旦亚界.见:王曰伦主编,中国震旦亚界.天津:天津科学技术出版社,1980,288~313
和政军,牛宝贵,张新元,等.2011a.北京密云元古宙常州沟组之下环斑花岗岩古风化壳岩石的发现及其碎屑锆石年龄.地质通报.30(5):798~802
和政军,张新元,牛宝贵,等.北京密云元古宙环斑花岗岩古风化壳及其与长城系常州沟组的关系．地学前缘,2011b.18(4):123~130
洪大卫.密云沙场环斑花岗岩的岩石学研究.北京大学研究生毕业论文，1965
侯贵廷.华北基性岩墙群.北京：科学出版社，2012
侯可军,李延河,邹天人,等. LA-MC-ICPMS锆石Hf同位素的分析方法及地质应用.岩石学报,2007,23(10):2595~2604
侯万荣,肖荣阁,张汉成,等.熊耳裂谷火山岩系金-多金属矿床成矿模式.黄金地质,2003,9:22~27
胡波,翟明国,郭敬辉,等.华北克拉通北缘化德群中碎屑锆石的LA-ICP-MS U-Pb年龄及其构造意义.岩石学报.2009.25(1):193~211
胡波,翟明国,彭澎,等.华北克拉通古元古代末~新元古代地质事件——来自北京西山地区寒武系和侏罗系碎屑锆石LA-ICP-MS U-Pb年代学的证据.岩石学报,2013,29(7):2508~2536
胡俊良,赵太平,徐勇航,等.华北克拉通大红峪组高钾火山岩的地球化学特征及其岩石成因.矿物岩石,2007,27(4):70~77
胡世玲,王松山,桑海清,等.大庙斜长岩同位素地质年龄、稀土地球化学及其地质意义.地质科学,1990,4:332~341
解广轰.大庙斜长岩杂岩体的岩石学特征.地球化学,1980,3:263~280
解广轰,王俊文.大庙斜长岩杂岩体侵位年龄的初步研究.地球化学,1988,1:13-17
解广轰.大庙斜长岩和密云环斑花岗岩的岩石学和地球化学——兼论全球岩体型斜长岩和环斑花岗岩类的时空分布及其意义.北京:科学出版社,2005
李怀坤,李惠民,陆松年.长城系团山子组火山岩颗粒锆石U-Pb年龄及其地质意义.地球化学,1995,24(1):43~48
李怀坤,陆松年,李惠民,等.侵入下马岭组的基性岩床的锆石和斜锆石U-Pb精确定年——对华北中元古界地层划分方案的制约.地质通报,2009,28(10):1396~1404
李怀坤,苏文博,周红英,等.华北克拉通北部长城系底界年龄小于1670Ma——来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMS U-Pb年龄的约束.地学前缘,2011,18(3):108~120
李怀坤,朱士兴,相振群,等.北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束.岩石学报,2010,26(7):2131~2140
李江海,侯贵廷,钱祥麟,等.恒山中元古代早期基性岩墙群的单颗锆石U-Pb年龄及其克拉通构造演化意义.地质论评,2001,47(3):234~238
李云,彭澎,王欣平.华北莱芜地区1680Ma基性岩墙群的特征及其地质意义.2013年全国岩石学与地球动力学研讨会(摘要),2013,136
刘敦一,万渝生,伍家善,等.华北克拉通太古宙地壳演化和最古老的岩石.地质通报,2007,26(9):1131~1138
刘兰笙,高翔,杜安道,等.白云鄂博稀土矿床中辉钼矿的铼-锇同位素年龄.矿床地质,1996,15(2):188~191
刘铁庚,张正伟,叶霖,等.白云鄂博“白云岩”地质地球化学特征及成因讨论,2012,86(5):723~734
刘铁庚.白云鄂博白云岩氧,碳同位素组成及其成因讨论.地质论评,1986,32(2):150~159
刘玉龙,陈江峰,李惠民,等.白云鄂博矿床白云石型矿石中独居石单颗粒U-Th-Pb-Sm-Nd定年.岩石学报,2005a,21(3):881~888
刘玉龙,杨刚,陈江峰,等.白云鄂博超大型稀土-铌-铁矿床黄铁矿Re-Os定年.科学通报,2005b,50(2):172~175
刘玉龙,陈江峰,李惠民,等.白云鄂博矿田碳酸岩墙年代学再研究.地质论评,2006,52(3):415~422
卢冰.大庙斜长岩及其中赋存的黑山铁磷矿床的地球化学.中国科学院广州地球化学研究所博士后出站报告,1995
陆松年,李怀坤,李惠民,等.华北克拉通南缘龙王□碱性花岗岩U-Pb年龄及其地质意义.地质通报,2003,22(10):762~768
陆松年,李惠民.蓟县长城系大红峪组火山岩中锆石精确定年.中国地质科学院院报,1991,22:137~145
陆松年,陈志宏,相振群.泰山世界地质公园古老侵入岩系年代格架.北京:地质出版社,2008,1~90
陆松年,相振群,李怀坤,等.华北克拉通对罗迪尼亚超大陆事件的响应——GOSEN连接假设.地质学报,2012,86(9):1396~1406
陆松年,杨春亮,李怀坤,等.华北古大陆与哥伦比亚超大陆.地学前缘,2002,9(4):225~233
孟庆润, Drew LJ.内蒙白云鄂博“H8含矿白云岩”氧、碳同位素研究及其成因.地质找矿论丛,1992,7(2):46~54
孟庆润.论白云鄂博铁矿含矿围岩——白云岩的沉积成因及其沉积环境分析.地质论评,1982,28(5):481~488
孟宪家,苏振东,包智强,等.白云鄂博群和渣尔泰群的地层和时代对比.中国地质科学院天津地质矿产研究所所刊,1988,20号:32~40
裴福萍,叶轶凡,王枫,等.吉林通化地区中元古代辉绿岩墙的发现及其地质意义.吉林大学学报(地球科学版),2013,43(1):100~108
彭澎,刘富,翟明国,等.密云岩墙群的时代及其对长城系底界年龄的制约.科学通报,2011,56(35):2975~2980
彭澎,翟明国,张华锋,等.华北克拉通1.8Ga镁铁质岩墙群的地球化学特征及其地质意义:以晋冀蒙交界地区为例.岩石学报,2004,20(3):439~456
彭润民,翟裕生,王建平,等.内蒙古狼山新古生代酸性火山岩的发现及其地质意义,科学通报,2010,55(26):2611-2620
彭润民,翟裕生.内蒙古东升庙矿区狼山群中变质“双峰式”火山岩夹层的确认及其意义.地球科学—中国地质大学学报,1997,22(6):589~594
乔秀夫,高林志,彭阳,等.内蒙古腮林忽洞群综合地层和白云鄂博矿床赋矿微晶丘.地质学报,1997,71(3):202-211
乔秀夫,姚培毅,王成述,等.内蒙古渣尔泰群层序地层及构造环境.地质学报,1991,1:1-16
裘愉卓.白云鄂博独居石SHRIMP定年的思考.地球学报,1997,18(S1):211~213
全国地层委员会.中国地层指南及中国地层指南说明书(修订版).北京:地质出版社,2013
任英忱,张英臣,张宗清.白云鄂博稀土超大型矿床的成矿时代及其主要地质热事件.地球学报,1994,15(S1):95~101
邵济安,翟明国,张履桥,等.晋冀蒙交界地区五期岩墙群的界定及其构造意义.地质学报,2005,79(1):56~67
沈保丰,翟安民,陈文明,等.中国前寒武纪成矿作用.北京:地质出版社,2006
宋彪.密云环斑花岗岩的同位素地质年代学、稀土地球化学特征及讨论.中国地质科学院地质研究所所刊,1992,25:137~156
苏文博,李怀坤, Huff WD,等.铁岭组钾质斑脱岩锆石SHRIMP U-Pb年代学研究及其地质意义.科学通报,2010,55(22):2197~2206
苏文博,李怀坤,徐莉,等.华北克拉通南缘洛峪群－汝阳群属于中元古界长城系——河南汝州洛峪口组层凝灰岩锆石LA-MC-ICP MS U-Pb年龄的直接约束.地质调查与研究,2012,35(2):96~108
孙会一,高林志,包创,等.河北宽城中元古代串岭沟组凝灰岩SHRIMP锆石U-Pb年龄及其地质意义.地质学报,2013,87(4):591~596
孙剑,朱祥坤,陈岳龙,等.白云鄂博地区相关地质单元的铁同位素特征及其对白云鄂博矿床成因的制约.2012,86(5):819~828
孙静,杜维河,王德忠,等.河北承德大庙黑山钒钛磁体矿床地质特征与成因探讨.地质学报,2009,83(9):1344~1364
孙枢,张国伟,陈志明.华北断块地区南部前寒武纪地质演化.北京:冶金工业出版社,1985
孙淑芬.内蒙古白云鄂博群尖山组微古植物新发现.地质论评,1992,38(5):474-480
万方晓.北京密云沙厂环斑花岗岩球斑结构的特征及成因探讨.北京地质,1994,3:17~23
万渝生,刘敦一,董春艳,等.中国最老岩石和锆石.岩石学报,2009,25(8):1793~1807
万渝生,刘敦一,殷小艳,等.鞍山地区铁架山花岗岩及表壳岩的锆石SHRIMP年代学和Hf同位素组成.岩石学报,2007,23(02):241~252
万渝生,宋彪,刘敦一,等.鞍山东山风景区3.8~2.5Ga古老岩带的同位素地质年代学和地球化学.地质学报,2001,75(3):363~370
万渝生,张巧大,宋天锐.北京十三陵长城系常州沟组碎屑钻石SHRIMP年龄:华北克拉通盖层物源区及最大沉积年龄的限定.科学通报,2003,48(18):1970~1975
王关玉.河北承德地区斜长岩体的岩石及矿床成矿特征.河北地质情报,1994,4:1-28
王惠初,相振群,赵凤清,等.内蒙古固阳东部碱性侵入岩:年代学、成因与地质意义.岩石学报,2012,28(9):2843~2854
王楫,李双庆,王保良,等.狼山~白云鄂博裂谷系.北京:北京大学出版社,1992
王凯怡,范宏瑞,谢奕汉,等.白云鄂博超大型REE~Fe~Nb矿产基底杂岩的锆石U-Pb年龄.科学通报,2001,46(16):1390~1394
王凯怡,杨奎峰,范宏瑞,等.白云鄂博矿床研究若干问题的探讨,2012,86(5):683~686
魏菊英,蒋少涌,万德芳.内蒙古白云鄂博稀土、铁矿床的硅同位素组成.地球学报,1994,15(1~2):102~110
魏菊英,上官志冠.白云鄂博铁矿围岩白云岩的氧、碳同位素组成及其成因//岩石学研究(第二辑).北京:地质出版社,1983,14~21
吴福元,李献华,郑永飞,等. Lu-Hf同位素体系及其岩石学应用.岩石学报,2007,23(2):185~220
相振群,李怀坤,陆松年,等.泰山地区古元古代末期基性岩墙形成时代厘定——斜锆石U-Pb精确定年.岩石学报,2012,28(9):2831~2842
肖荣阁,费红彩,王安建,等.白云鄂博含矿碱性火山岩建造及其地球化学,2012,86(5):735~752
邢长明,陈伟,王焰,等.华北克拉通北缘元古宙大庙Fe-Ti-P矿床的挥发份组成和C~H~O同位素研究.岩石学报,27(05):1500~1510
徐德斌,白志达,王敦则,等.河北省兴隆地区大红峪组沉积古环境研究.地层学杂志,2002,26(1):73~79
徐平,吴福元,谢烈文,等. U-Pb同位素定年标准锆石的Hf同位素.科学通报,2004.49:1403~1410
阎国翰,郭立鹤,钱彬.承德黑山苏长岩中斜长石研究.北京大学地质系“研究生论文集”,北京:北京大学出版社,1985,106~114
阎国翰,牟保磊.承德黑山斜长杂岩体辉石特征及其形成温度条件.岩石学报,1993,9(3):300~307
杨进辉,吴福元,柳小明,等.北京密云环斑花岗岩锆石U-Pb年龄和Hf同位素及地质意义.岩石学报,2005,21(6):1633~1644
杨奎锋,范宏瑞,胡芳芳,等.白云鄂博陆缘裂谷系沉积物源与超大型稀土矿床含矿白云岩的成因探讨.2012,86(5):775~784
杨岳衡,孙金凤,谢烈文,等.地质样品Nd同位素激光原位等离子体质谱(LA-MC-ICPMS)测定.科学通报,2008.53(5):568~576
郁建华.北京及附近元古宙裂谷槽中球斑花岗岩套的地球化学.地质学报,1990,64(4):322~336
郁建华,付会芹, I.哈巴拉,等.华北克拉通北部1.70Ga非造山环斑花岗岩岩套.华北地质矿产杂志,1996,11(3):9~18
郁建华,付会芹,张凤兰,等.华北地台北部非造山环斑花岗岩及有关岩石.北京:中国科学技术出版社,1996,1~182
袁忠信.再谈白云鄂博矿床的成矿时代和矿床成因.2012,86(5):683~686
翟明国,卞爱国.华北克拉通新太古代末超大陆拼合及古元古代末—中元古代裂解.中国科学(D辑),2000,30:129~137
翟明国,胡波,彭澎,等.华北中~新元古代的岩浆作用与多期裂谷事件.地学前缘,2014,21(1):100~119
翟明国,彭澎.华北克拉通古元古代构造事件.岩石学报,2007,23(11):2665~2682
翟明国.华北克拉通2.1~1.7Ga地质事件群的分解和构造意义探讨.岩石学报,2004.20(6):1343~1354
翟明国.华北克拉通的形成演化与成矿作用.矿床地质,2010,29(1):24~36
翟裕生.某斜长岩的岩石特征及成因.地质论评,1965,23(3):186~195
张汉成,肖荣阁,安国英,等.熊耳群火山岩系金银多金属矿床热水成矿作用.中国地质,2003,34(4):400~405
张华锋,周志广,刘文灿,等.内蒙古中部白乃庙地区格林威尔岩浆事件记录:石英二长闪长岩脉锆石LA-ICP-MS U-Pb年龄证据.岩石学报,2009,25:1512~1518
张鹏远,牛绍武,王长尧,等.白云鄂博地区地质构造特征.中国地质科学院天津地质研究所所刊(第28号).北京:地质出版社,1993,1~86
张拴宏,赵越,叶浩,等.燕辽地区长城系串岭沟组及团山子组沉积时代的新制约.岩石学报.2013,29(07):2481~2490
张维,张福斌,张天龙,等.在第四系覆盖区重磁异常上如何辨别基性岩体与铁矿异常.地质调查与研究,2014
张宗清,唐索寒,王进辉,等.白云鄂博稀土矿床形成年龄的新数据.地球学报,1994,15(1~2):85~94.
张宗清,袁忠信,唐索寒,等.白云鄂博矿床年龄和地球化学.北京:地质出版社,2003
章雨旭,吕洪波,王俊,等.白云鄂博矿床成矿构造环境分析.2012,86(5):767~774
章雨旭,吕洪波,张绮玲,等.微晶丘成因新认识.地球科学进展,2005,20(6):693~700
章雨旭,彭阳,乔秀夫,等.白云鄂博矿床赋矿白云岩成因新认识.地质论评,1998,44(1):70~76.
章雨旭,杨占峰,张绮玲,等.白云鄂博矿床及北京西山微晶丘地质、地球化学研究.北京:地质出版社,2009
赵崇贺.北京密云斜长环斑花岗岩地质学和岩石学研究.第一届矿物岩石地球化学学术会议论文集——岩石部分.北京:科学出版社,1964,124~143
赵太平,陈福坤,翟明国,等.河北大庙斜长岩杂岩体锆石U–Pb年龄及其地质意义.岩石学报.2004b.20(3):685~690
赵太平.华北陆块元古宙熊耳群火山岩、大庙斜长岩杂岩岩体的年代学、岩石地球化学与构造环境研究.中国科学院广州地球化学研究所博士后出站报告,2003
赵太平,金成伟,翟明国,等.华北陆块南部熊耳群火山岩的地球化学特征与成因.岩石学报,2002,18(1):59~69
赵太平,王建平,张忠慧,等.中国王屋山及邻区元古宙地质研究.北京:中国大地出版社,2005
赵太平,徐勇航,翟明国.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议.高校地质学报,2007,13(2):191~206
赵太平,翟明国,夏斌,等.熊耳群火山岩锆石SHRIMP年代学研究:对华北克拉通盖层发育初始时间的制约.科学通报,2004a,49(22):2342~2349
赵太平,周美夫,金成伟,等.华北陆块南缘熊耳群形成时代讨论.地质科学,2001,36(3):326~334
钟富道,解广轰,等.斜长岩事件年龄及其地质意义.地球化学,1978,3:202~208
周建波,郑永飞,杨晓勇,等.白云鄂博地区构造格局与古板块构造演化.高校地质学报,2002,8(1):46~61
周永昶,袁朝.大庙斜长岩杂岩体及铁磷矿的稀土元素地球化学研究.长春地质学院学报,1989,19(1):43~53
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.地质论评,1980,26(1):35~41
朱士兴,邢裕盛,张鹏远.华北地台中、上元古界生物地层序列.北京:地质出版社,1994
朱祥坤,孙剑.内蒙古白云鄂博矿床的稀土矿化时代与期次.地球学报,2012,33(6):845-855
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