中国地质调查局天津地质调查中心主办
高级检索

华北克拉通中北部麻粒岩带基础地质调查进展及相关问题讨论

,  ,  ,  ,  ,  , 

文章导航 > 华北地质 > 2022 > 45(1): 18-41

上一篇

下一篇

王惠初, 张家辉, 任云伟, 施建荣, 相振群, 常青松, 王智. 2022. 华北克拉通中北部麻粒岩带基础地质调查进展及相关问题讨论[J]. 华北地质, 45(1): 18-41. doi: 10.19948/j.12-1471/P.2022.01.02
引用本文: 王惠初, 张家辉, 任云伟, 施建荣, 相振群, 常青松, 王智. 2022. 华北克拉通中北部麻粒岩带基础地质调查进展及相关问题讨论[J]. 华北地质, 45(1): 18-41. doi: 10.19948/j.12-1471/P.2022.01.02
shu
WANG Hui-chu, ZHANG Jia-hui, REN Yun-wei, SHI Jian-rong, XIANG Zhen-qun, CHANG Qing-song, WANG Zhi. 2022. Geological survey of granulite belt in the north-central part of North China Craton:progress and discussion on related problems. North China Geology, 45(1): 18-41. doi: 10.19948/j.12-1471/P.2022.01.02
Citation: WANG Hui-chu, ZHANG Jia-hui, REN Yun-wei, SHI Jian-rong, XIANG Zhen-qun, CHANG Qing-song, WANG Zhi. 2022. Geological survey of granulite belt in the north-central part of North China Craton:progress and discussion on related problems. North China Geology, 45(1): 18-41. doi: 10.19948/j.12-1471/P.2022.01.02
shu

华北克拉通中北部麻粒岩带基础地质调查进展及相关问题讨论

  • 1. 中国地质调查局天津地质调查中心, 天津 300170;

  • 2. 中国地质调查局前寒武纪地质研究中心, 天津 300170;

  • 3. 中国地质调查局国际矿业研究中心, 北京 100037

  • 基金项目:

    中国地质调查局项目：“燕山-太行成矿带丰宁和天镇地区地质矿产调查（DD20160042）”；“河北怀安-内蒙古凉城地区区域地质调查（DD20190035）”；国家青年科学基金项目（41902196）联合资助

详细信息
    作者简介: 王惠初(1963-),男,研究员,从事前寒武纪地质与区域地质调查研究;E-mai l:tjwhui chu@163.com

  • 中图分类号: P588.3;P542

Geological survey of granulite belt in the north-central part of North China Craton:progress and discussion on related problems

  • 1. Tianjin Center, China Geological Survey, Tianjin 300170, China;

  • 2. Precambrain Geological Research Centre, China Geological Survey, Tianjin 300170, China;

  • 3. International Mining Research Center, China Geological Survey, Beijing 100037, China

    摘要
  • 华北克拉通中北部麻粒岩带被认为是古元古代造山带，晋冀蒙相邻地区的高压麻粒岩和超高温变质岩吸引了国内外早前寒武纪地质学家的目光。本文以区域地质调查资料为基础，重新厘定了华北克拉通中北部的构造单元，自北向南依次划分为阴山新太古代岩浆弧（阴山地块）、乌拉山-大青山古元古代再造杂岩带（Pt 1）、凉城深熔花岗岩带（Pt 1）、天镇-怀安再造杂岩带（Pt 1）和五台新太古代岛弧带。梳理了古元古代造山带三个构造单元的地层系统和主要构造热事件，认为乌拉山-大青山古元古代再造杂岩带和天镇-怀安再造杂岩带在物质组成和构造热事件记录上具有可比性。通过地质填图，将凉城深熔花岗岩划分为3期6种岩石类型，并发现了不含石榴石的紫苏花岗闪长岩（石英闪长岩），具有钙碱性系列I型花岗岩特征。根据钻孔资料结合航磁特征探讨了鄂尔多斯盆地变质基底的构造属性，认为古元古代造山带的构造线切割了鄂尔多斯盆地基底，鄂尔多斯基底不是一个太古宙地块。综合分析古元古代变质作用、岩浆作用和构造变形作用，认为古元古代造山带经历了大陆裂解、俯冲碰撞、板片拆沉-地幔上涌、挤压造山和造山后伸展抬升的复杂演化过程，反映了早期热板块构造的特殊性。
    The granulite belt in the north-central North China Craton is considered to be a Paleoproterozoic orogenic belt.The high-pressure granulite and ultra-high temperature metamorphic rocks in the adjacent areas of Shanxi, Hebei and Inner Mongolia have attracted the attention of Early Precambrian geologists around the world.Based on the regional geological survey data, this paper redefines the tectonic unit in the north central part of the North China Craton, which is divided into Yinshan Neoarchean magmatic arc(Yinshan block), Daqingshan-Wulashan Paleoproterozoic reworking complex belt(Pt1), Liangcheng deep melt granite belt(Pt1), Tianzhen-Huai'an reworking complex belt(Pt1)and Wutai Neoarchean island-arc belt from north to south.The stratigraphic system and main tectonic thermal events in the three tectonic units of the Paleoproterozoic orogen are redefined.It is considered that the Daqingshan-Wulashan Paleoproterozoic and Tianzhen-Huai'an reworking complex belt are comparable in material composition and records of tectonic thermal events.Through geological mapping, the anatexis granite was formed in three stages and divided into six kinds of rock types, and Opxbearing granodiorite(quartz-diorite)without garnet is found, which is characterized by calc alkaline series I-type granite.Based on borehole data and aeromagnetic characteristics, the structural properties of metamorphic basement of Ordos Basin are discussed.It is considered that the tectonic line of the Paleoproterozoic orogenic belt cuts the basement of the Ordos Basin, and the Ordos basement is not an Archean block.Based on the comprehensive analysis of Paleoproterozoic metamorphism, magmatism and tectonic deformation, it is considered that the Paleoproterozoic orogenic belt has experienced the complex evolution process of continental breakup, subduction collision, plate delamination, mantle upwelling, compression orogeny and post orogenic extension and uplift, which reflects the particularity of Early hot-plate tectonics.
    • HTML全文
  • 加载中
    • 参考文献(179)
  • [1]

    ZHAI M G, SANTOSH M.The early Precambrian odyssey of North Cehina Craton:a synoptic overview[J].Gondwana Research, 2011, 20(1):6–25.

    [2]

    ZHAO G C, CAWOOD P A, WILDE S A, et al.Amalgamation of the North China Craton:key issues and discussion[J].Precambrian Research, 2012, 222-223:55-76.

    [3]

    沈其韩,徐惠芬,张宗清,等.中国早前寒武纪麻粒岩[J].北京:地质出版社,1992, 57-62.

    [4]

    翟明国,郭敬辉,闫月华,等.中国华北太古宙高压基性麻粒岩的发现及其初步研究[J].中国科学(B),1992,12:1325-1330.

    [5]

    ZHAI M G, GUO J H, YAN Y H, et l.Discovery of high pressure basic granulite terrain in North China Archean craton and preliminary study[J].Science China(Ser B), 1993, 36:1402-1408.

    [6]

    郭敬辉,翟明国,张毅刚,等.怀安蔓菁沟早前寒武纪高压麻粒岩混杂岩带地质特征,岩石学和同位素年代学[J].岩石学报,1993,9(4):329-341.

    [7]

    ZHAI M G, GUO J H, LI J H et al.Retrograded eclogites in the Archean North China craton and their geological implication[J].Chinese Sci Bull, 1996, 41:315-326.

    [8]

    GUO J, ZHAI M, XU R.Timing of the granulite facies metamorphism in the Sanggan area, North China craton:zircon UPb geochronology[J].Science in China Series D:Earth Sciences.2001, 44(11):1010-1018.

    [9]

    GUO J H, O’BRIEN P J, ZHAI M G.High pressure granulites in the Sanggan area, North China craton:metamorphic evolution, P-T paths and geotectonic significance[J].Journal of Metamorphic Geology, 2002, 20:741-756.

    [10]

    GUO J H, SUN M, CHEN F K, et al.Sm-Nd and SHRIMP U-Pb zircon geochronology of high pressure granulites in the Sanggan area, North China Craton:timing of Paleoproterozoic continental collision[J].Journanl of Asian Earth Sci, 2005, 24:629-642

    [11]

    马军,王仁民.宣化-郝城高压麻粒岩带中蓝晶石-正条纹长石组合的发现及地质意义[J].岩石学报,1995,11(3):273-278.

    [12]

    阎月华.大同孤山含石榴石麻粒岩的成因讨论[C].华北北部麻粒岩带地质演化[M].北京:地震出版社,1994,199-209.

    [13]

    ZHANG J, ZHAO G C, SUN M, et al.High-pressure mafic granulites in the Trans-North China Orogen:tectonic significance and age[J].Gondwana Research.2006, 9, 349-362.

    [14]

    毛德宝,钟长汀,陈志宏,等.承德北部高压麻粒岩的同位素年龄及其地质意义[J].岩石学报,1999,15(4):524-531.

    [15]

    ZHAO G C, WILDE S A, Cawood P A, et al.Thermal evolution of two types of mafic granulites from the North China craton:implications for both mantle plume and collisional tectonics[J].Geological Magazine, 1999, 136, 223-240.

    [16]

    ZHAO G C, CAWOOD P A, WILDE S A, et al.Metamorphism of basement rocks in the Central Zone of the North China Craton:implications for Paleoproterozoic tectonic evolution[J].Precambrian Research.2000, 103, 55-88.

    [17]

    ZHAO G C, Cawood P A, Wilde S A, et al.High-pressure granulites(retrograded eclogites)from the Hengshan Complex, North China Craton:petrology and tectonic implications[J].Journal of Petrology, 2001, 42(6):1141-1170.

    [18]

    YIN C Q, ZHAO G C, GUO J H, et al.U-Pb and Hf isotopic study of zircons of the Helanshan Complex:constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton[J].Lithos, 2011, 122, 25-38.

    [19]

    YIN C Q, ZHAO G C, WEI C J, et al.Metamorphism and partial melting of high-pressure pelitic granulites from the Qianlishan Complex:constraints on the tectonic evolution of the Khondalite Belt in the North China Craton[J].Precambrian Research.2014, 242, 172-186.

    [20]

    郭敬辉,陈意,彭澎,等.内蒙古大青山假蓝宝石麻粒岩-1.8 Ga的超高温(UHT)变质作用[C].《2006年全国岩石学与地球动力学研讨会论文摘要集》[R].南京,2006,215-218.

    [21]

    GUO J H, PENG P, CHEN Y, et al.UHT sapphirine granulite metamorphism at 1.93-1.92 Ga caused by gabbronorite intrusions:Implications for tectonic evolution of the northern margin of the North China Craton[J].Precambrian Research, 2012, 222-223:124-142.

    [22]

    SANTOSH M, WILDE S A, LI J H.Timing of Paleoproterozoic ultrahigh-temperature metamorphism in the North China Craton:Evidence from SHRIMP U-Pb zircon geochronology[J].Precambrian Research, 2007, 159:178-196.

    [23]

    SANTOSH M, SAJEEV K, LI J H, et al.Counterclockwise exhumation of a hot orogen:the Paleoproterozoic ultrahightemperature granulites in the North China Craton[J].Lithos, 2009, 110:140-152.

    [24]

    JIAO S H, GUO JH.Application of the two-feldspar geothermometer to ultrahigh-temperature(UHT)rocks in the Khondalite belt, North China craton and its implications[J].American Mineralogist, 2011, 96, 250-260.

    [25]

    LIU S J, TSUNOGAE T, LI W S, et al.Paleoproterozoic granulites from Heling’er:implications for regional ultrahigh-temperature metamorphism in the North China Craton[J].Lithos, 2012.148, 54-70.

    [26]

    白瑾,黄学光,王惠初,等.中国前寒武纪地壳演化(第二版)[M].北京:地质出版社,1996,1-259.

    [27]

    白瑾,王汝铮,郭进京.五台山早前寒武纪重大地质事件及其年代[M].北京:地质出版社,1992,1-52.

    [28]

    伍家善,耿元生,沈其韩,等.中朝古大陆太古宙地质特征及构造演化[M].北京:地质出版社,1998,192-211.

    [29]

    张福勤,刘建忠,欧阳自远.华北克拉通基底绿岩的岩石大地构造学研究[J].地球物理学报,1998,41:99-107.

    [30]

    邓晋福,吴宗絮,赵国春,等.华北地台前寒武纪花岗岩类、陆壳演化与克拉通形成[J].岩石学报,1999,15:190-198.

    [31]

    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[J].中国科学:地球科学,2000,30(S1):129-137.

    [32]

    翟明国.克拉通化与华北陆块的形成[J].中国科学:地球科学,2011,41(8):1037-1046.

    [33]

    ZHAO G C,CAWOOD P A,WILDE S A,et al.Metamorphism of basement rocks in the Central zone of the North China craton:implications for Paleoproterozoic tectonic evolution[J].Precambrian Research,2000,103(1-2):55-88.[34]ZHAO G C, WILDE S A, CAWOOD P A, et al.Archaean blocks and their boundaries in the North China craton:lithological, geochemical, structural and P-T path constraints and tectonic evolution[J].Precambrian Research, 2001, 107, 45-73.

    [35]

    ZHAO G C, SUN M, WILDE S A, et al.Late Archean to Paleoproterozoic evolution of the North China Craton:Key issues revisited[J].Precambrian Research, 2005, 136:177-202.

    [36]

    ZHAO G C, ZHAI M G.Lithotectonic elements of Precambrian basement in the North China Craton:Review and tectonic implications[J].Gondwana Research, 2013, 23(4):1207-1240.

    [37]

    赵国春.华北克拉通基底主要构造单元变质作用演化及其若干问题讨论[J].岩石学报,2009,25(8):1772-1792.

    [38]

    KUSKY T M AND LI J H.Paleoproterozoic tectonic evolution of the North China Craton[J].Journal of Asian Earth Sciences, 2003, 22(4):383-397.

    [39]

    KUSKY T M,LI J H, SANTOSH M.The Paleoproterozoic North Hebei Orogen:North China Craton’s collisional suture with the Columbia supercontinent[J].Gondwana Research, 2007, 12(1-2):4-28.

    [40]

    陆松年,郝国杰,王惠初,等.中国变质岩大地构造图及说明书[M].地质出版社,2015,1-92.

    [41]

    陆松年,郝国杰,王惠初,等.中国变质岩大地构造研究[M].地质出版社,2017,1-338.

    [42]

    任云伟,施建荣,李杰,等.凉城幅地质图(1/50000)[R].中国地质调查局天津地质调查中心,2021.

    [43]

    王智,王惠初,施建荣,等.内蒙古集宁地区徐武家变质辉长岩的形成背景及其地质意义[J].地质调查与研究,2020,43(2):97-113.

    [44]

    内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社,1991,1-725.

    [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,1996,1-142.

    [46]

    卢良兆,徐学纯,刘福来.中国北方早前寒武纪孔兹岩系[M].长春:长春出版社,1996, 1-125.

    [47]

    金巍,李树勋,刘喜山.内蒙大青山地区早前寒武纪高级变质岩系特征和变质动力学[J].岩石学报,1991,7(4):27-35.

    [48]

    金巍,李树勋.内蒙古大青山地区早元古宙造山带的岩石组成及特征[C].华北北部麻粒岩带地质演化[M].北京:地震出版社, 1994.

    [49]

    刘喜山.大青山造山带中基底再造杂岩的特征及其指示意义[J].岩石学报,1994,10(4):413-426.

    [50]

    钱祥麟,崔文元,王时麒.内蒙-冀东太古界麻粒岩相带的演化[C].地质科学论文集[M].北京:北京大学出版社,1985,20-29.

    [51]

    沈其韩,张荫芳,高吉凤,等.内蒙古中南部太古宙变质岩[J].中国地质科学院地质研究所所刊,1990,21:1-192.

    [52]

    赵宗溥.中朝准地台前寒武纪地壳演化[M].北京:科学出版社,1993,1-444.

    [53]

    钱祥麟,李江海.华北克拉通新太古代不整合事件的确定及其大陆克拉通构造演化意义[J].中国科学(D辑:地球科学),1999,(01):1-8.

    [54]

    杨振升,徐仲元,刘正宏.孔兹岩系事件与太古宙地壳构造演化[J].前寒武纪研究进展,2000,23(4):206-212.

    [55]

    杨振升,徐仲元,刘正宏,等.高级变质岩石地层系统建立的思考与实践-以内蒙古大青山-乌拉山地区为例[J].中国地质,2003,4:343-351.

    [56]

    杨振升,徐仲元,刘正宏,等.内蒙古中部大青山-乌拉山地区早前寒武系研究的重要进展及对高级变质区开展地层工作的几点建议[J].地质通报,2006,25(4):427-433.

    [57]

    徐仲元,刘正宏,杨振升.内蒙古大青山地区早前寒武纪变质地层的组成及特征[J].世界地质,2001,3:209-218.

    [58]

    徐仲元, 刘正宏, 杨振升.内蒙古大青山地区孔兹岩系的地层结构[J].吉林大学学报(地球科学版),2002,32(4):209-218.

    [59]

    徐仲元,刘正宏,杨振升,等.内蒙古中部大青山-乌拉山地区孔兹岩系的变质地层结构及动力学意义[J].地质通报,2007,26(5):526-536.

    [60]

    吴昌华,孙敏,李惠民,等.乌拉山-集宁孔兹岩锆石激光探针等离子质谱(LA-ICP-MS)年龄-孔兹岩沉积时限的年代学研究[J].岩石学报,2006,22(11):2639-2654.

    [61]

    WAN Y S, SONG B, LIU D Y, et al.SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary rocks in the North China Craton:evidence for a major Late Palaeoproterozoic tectonothermal event[J].Precambrian Research.2006, 149, 249-271.

    [62]

    WAN Y S, LIU D Y, DONG C Y, et al.The Precambrian Khondalite Belt in the Daqingshan area, North China Craton:evidence for multiple metamorphic events in the Palaeoproterozoic[J].In:Reddy, S.M., Mazumder, R., Evans, D.A.D., Collins, A.S.(Eds.), Palaeoproterozoic Supercontinents and Global Evolution, 323.Geological Society, Special Publications, London, 2009, 73-97.

    [63]

    ZHAO G C, CAWOOD P A.Precambrian geology of China[J].Precambrian Research, 2012, 222-223:13-54.

    [64]

    董春艳,万渝生,徐仲元,等.华北克拉通大青山地区古元古代晚期孔兹岩系:锆石SHRIMP U-Pb定年[J].中国科学(D辑),2012,42(12):1851-1862.

    [65]

    DONG C Y, WAN Y S, XU Z Y, et al.Late Paleoproterozoic khondalites in the Daqingshan area, North China Craton:SHRIMP zircon U-Pb dating[J].Science in China Series D Earth Sciences, 2013, 56, 115-125.

    [66]

    马铭株,董春艳,徐仲元,等.内蒙古大青山地区古元古代早期榴云片麻岩(大青山表壳岩)深熔作用:地质、锆石年代学和地球化学研究[J].岩石学报,2015,31(6):1535-1548.

    [67]

    PENG P, WANG X, WINDLEY BF, et al.Spatial distribution of-1950-1800 Ma metamorphic events in the North China Craton:Implications for tectonic subdivision of the craton[J].Lithos, 2014, 202-203:250-266.

    [68]

    蔡佳,刘福来,刘平华,等.内蒙古孔兹岩带乌拉山-大青山地区古元古代孔兹岩系年代学研究[J].岩石学报,2015,31(10):3081-3106.

    [69]

    钟焱,陈雅丽,翟明国,等.华北克拉通西部古元古代孔兹岩系的地层对比、岩相古地理特征及其地质意义[J].岩石学报,2016,32(3):713-726.

    [70]

    李璞,钟富道.集宁地区变质岩系的初步划分及其变质相的探讨[J].地质科学,1965,6(1):1-14.

    [71]

    董启贤,周俊昌.内蒙古乌拉山区原乌拉山群地层划分新议[J].中国区域地质,1984,(10):19-37.

    [72]

    JIAO S J, GUO J H, HARLEY S L, et al.Geochronology and trace element geochemistry of zircon, monazite and garnet from the garnetite and/or associated other high-grade rocks:Implications for Palaeoproterozoic tectonothermal evolution of the Khondalite Belt, North China Craton[J].Precambrian Research, 2013, 237:78-100.

    [73]

    WANG L J, GUO J H, PENG P, et al.Lithological units at the boundary zone between the Jining and Huai’an Complexes(central-northern margin of the North China Craton):a Paleoproterozoic tectonic mélange[J].Lithos, 2015, 227, 205-224.

    [74]

    CAI J, LIU F, LIU P.Paleoproterozoic multistage metamorphic events in Jining metapelitic rocks from the Khondalite Belt in the North China Craton:Evidence from petrology, phase equilibria modelling and U-Pb geochronology[J].Journal of Asian Earth Sciences, 2017, 138:515-534.

    [75]

    赵宗溥.中国前寒武纪地层问题[J].地质学报,1954,34(2):169-196.

    [76]

    刘宇光,郭敬辉.冀西北地区早前寒武纪地质[C]//中朝准地台前寒武纪地壳演化[M].北京:科学出版社,1993,284-330.[77]刘宇光.中国冀西北及邻区早前寒武纪变质杂岩的成因和地壳演化:岩石学、地球化学、同位素地质年代学研究[D].中国地质科学院,1989.

    [78]

    河北省地质调查院,张家口市幅(1/250000)区域地质调查报告[R].2005.

    [79]

    山西省地质调查院.大同市幅(1/250000)区域地质调查报告[R].2014.

    [80]

    XIA X P, SUN M, ZHAO G C, et al.LA-ICP-MS U-Pb geochronology of detrital zircons from the Jining Complex, North China Craton and its tectonic significance[J].Precambrian Research, 2006, 144(3):199-212.

    [81]

    WANG J, WU Y B, GAO S, et al.Zircon U-Pb and Trace Element Data from Rocks of the Huai'an Complex:New Insights into the Late Paleoproterozoic Collision between the Eastern and Western Blocks of the North China Craton[J].Precambrian Research, 2010, 178(1-4):59-71.

    [82]

    ZHAO G C, WILDE S A, SUN M, et al.SHRIMP U-Pb zircon geochronology of the Huai'an Complex:Constraints on Late Archean to Paleoproterozoic magmatic and metamorphic events in the Trans-North China Orogen[J].American Journal of Science, 2008, 308(3):270-303.

    [83]

    ZHAO G C, WILDE S A, GUO J H.Single Zircon Grains Record Two Paleoproterozoic Collisional Events in the North China Craton[J].Precambrian Research, 2010, 177:266-276.

    [84]

    张家辉,田辉,王惠初,等.华北克拉通怀安杂岩中早前寒武纪两期变质表壳岩的重新厘定:岩石学及锆石U-Pb年代学证据[J].地球科学,2019,44(01):1-22.

    [85]

    王仁民,陈珍珍,陈飞.恒山灰色片麻岩和高压麻粒岩包体及其地质意义[J].岩石学报,1991,7(4):36-45.

    [86]

    郭敬辉,翟明国,李江海,等.华北克拉通早前寒武纪桑干构造带的岩石组合特征和构造性质[J].岩石学报,1996,12(2):193-207.

    [87]

    张家辉,王惠初,田辉,等.华北克拉通怀安杂岩中“MORB”型高压基性麻粒岩的成因及其构造意义[J].岩石学报,2019,35(11):3506-3528.

    [88]

    PENG P, GUO J H, WINDLEY B F, et al.Halaqin volcanosedimentary succession in the central-northern margin of the North China Craton:Products of Late Paleoproterozoic ridge subduction[J].Precambrian Research, 2011, 187(1-2):165-180.

    [89]

    HUANG G, JIAO S, GUO J, et al.P-T-t constraints of the Barrovian-type metamorphic series in the Khondalite belt of the North China Craton:Evidence from phase equilibria modeling and zircon U-Pb geochronology[J].Precambrian Research, 2016, 283:125-143.

    [90]

    BROWN M, RUSHMER T.(eds)Evolution and Differentiation of the Continental Crust[M].Cambridge, New York, Melbourne:Cambridge University Press, 2006, 1-553.

    [91]

    CLEMENS J D.Melting of the continental crust:fluid regimes, melting reactions, and source-rock fertility.In:Brown M, Rushmer T.(Eds.), Evolution and Differentiation of the Continental Crust[M].Cambridge University Press, Cambridge, UK, 2006, 297-331.

    [92]

    CHAPPELL B W, WHITE A J R.Two contrasting granite types:25 years later[J].Australian Journal of Earth Sciences, 2001, 48(4):489-499.

    [93]

    PENG P, GUO J H, ZHAI M G, et al.Paleoproterozoic gabbronoritic and granitic magmatism in the northern margin of the North China craton:Evidence of crust-mantle interaction[J].Precambrian Research, 2010, 183(3):635-659.

    [94]

    PENG P, GUO J H, WINDLEY B F, et al.Petrogenesis of Late Paleoproterozoic Liangcheng charnockites and S-type granites in the centralnorthern margin of the North China Craton:implications for ridge subduction[J].Precambrian.Research, 2012, 222-223, 107-123.

    [95]

    ZHAI M G, LIU W J.Paleoproterozoic tectonic history of the North China Craton:a review[J].Precambrian Research, 2003, 122:183-199.

    [96]

    钟长汀,邓晋福,万渝生,等.华北克拉通北缘中段古元古代造山作用的岩浆记录:S型花岗岩地球化学特征及锆石SHRIMP年龄[J].地球化学,2007,36(06):633-637.

    [97]

    LI X W, WEI C J.Ultrahigh-temperature metamorphism in the Tuguiwula area, Khondalite Belt, North China Craton[J].Journal of Metamorphic Geology, 2018, 36(4):489-509.

    [98]

    WANG L J, GUO J H, YIN C Q, et al.Petrogenesis of ca.1.95 Ga meta-leucogranites from the Jining Complex in the Khondalite Belt, North China Craton:Water-fluxed melting of metasedimentary rocks[J].Precambrian Research, 2017:355-371.

    [99]

    WANG L J, GUO J H, YIN C Q, et al.High-temperature Stype granitoids(charnockites)in the Jining complex, North China Craton:Restite entrainment and hybridization with mafic magma[J].Lithos, 2018, 320-321:435-453.

    [100]

    石强,董晓杰,徐仲元,等.华北地台北缘集宁地区古元古代片麻状石榴花岗岩的深熔成因及地质意义[J].岩石学报,2018,34(09):2754-2772.

    [101]

    常青松,王惠初,施建荣,等.集宁地区两类古元古代重熔花岗岩的锆石U-Pb年代学及岩石成因[J].地球科学,2020,45(9):3258-3267.

    [102]

    王洛娟,郭敬辉,彭澎.华北克拉通孔兹岩带古元古代凉城石榴石花岗岩成因机制及其岩石学意义[J].岩石学报,2021,37(02):375-390.

    [103]

    钟长汀.华北克拉通北缘中段古元古代花岗岩类地球化学、年代学与构造意义[D].中国地质大学(北京),2006,1-194.

    [104]

    PAT I O DOUCE A E.What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas?[J].Geological Society, London, Special Publications, 1999, 168, 55-75.

    [105]

    翟明国.鄂尔多斯地块是破解华北早期大陆形成演化和构造体制谜团的钥匙[J].科学通报,2021,66:3441-3461.

    [106]

    邓军,王庆飞,黄定华,等.鄂尔多斯盆地基底演化及其对盖层控制作用[J].地学前缘,2005,3:91-99.

    [107]

    贾进斗,何国琦,李茂松,等.鄂尔多斯盆地基底结构特征及其对古生界天然气的控制[J].高校地质学报,1997,2:17-26.

    [108]

    张抗.鄂尔多斯断块构造和资源[M].西安:陕西科学技术出版社,1989,1-394.

    [109]

    刘正宏,徐仲元,杨振升,等.鄂尔多斯北缘石合拉沟逆冲推覆构造的发现及意义[J].地质调查与研究,2004,27(1):24-27.

    [110]

    邸领军.鄂尔多斯盆地基底演化及沉积盖层相关问题的控究[D].西北大学博士论文,2003,157.

    [111]

    ZHANG C L, DIWU C R, KRÖNER A, et al.Archean-Paleoproterozoic crustal evolution of the Ordos Block in the North China Craton:Constraints from zircon U-Pb geochronology and Hf isotopes for gneissic granitoids of the basement[J].Precambrian Research,2015, 267:121-136.

    [112]

    WANG WR, LIU X, HU J, et al.Late Paleoproterozoic medium-P high grade metamorphism of basement rocks beneath the northern margin of the Ordos Basin, NW China:Petrology, phase equilibrium modelling and U-Pb geochronology[J].Precambrian Res, 2014, 251:181-196.

    [113]

    WAN Y S, XIE H Q, YANG H, et al.Is the Ordos Block Archean or Paleoproterozoic in age?Implications for the Precambrian evolution of the North China Craton[J].American Journal of Science,2013,313, 683-711.

    [114]

    WANG W R, ZHAO Y, LIU X, et al.Metamorphism of diverse basement gneisses of the Ordos Basin:Record of multistage Paleoproterozoic orogenesis and constraints on the evolution of the western North China Craton[J].Precambrian Research, 2019, 328:48-63.

    [115]

    胡健民,刘新社,李振宏,等.鄂尔多斯盆地基底变质岩与花岗岩锆石SHRIMP U-Pb定年[J].科学通报,2012,57(26):2482-2491.

    [116]

    吴素娟,张永生,邢恩袁.鄂尔多斯盆地变质基底中碎屑锆石的LA-ICP-MS U-Pb年龄及其构造意义[J].地质学报, 2015, 89:2171-2186.

    [117]

    高山林,林晋炎,陆彦俊.宁夏泾源石咀子古元古代A型花岗岩的形成时代及其地质意义[J].岩石学报,2013,29(08):2676-2684.

    [118]

    SU Y, ZHENG J, GRIFFIN W L, et al.Zircon U-Pb ages and Hf isotope of gneissic rocks from the Huai’an Complex:Implications for crustal accretion and tectonic evolution in the northern margin of the North China Craton[J].Precambrian Research,2014, 255:335-354.

    [119]

    LIAO Y, WEI C.Ultrahigh-temperature mafic granulite in the Huai'an Complex, North China Craton:Evidence from phase equilibria modelling and amphibole thermometers[J].Gondwana Research, 2019, 76:62-76.

    [120]

    ZHANG H, ZHAI M, SANTOSH M, et al.Paleoproterozoic granulites from the Xinghe graphite mine, North China Craton:Geology, zircon U-Pb geochronology and implications for the timing of deformation, mineralization and metamorphism[J].Ore Geology Reviews,2014, 63:478-497.

    [121]

    WANG H Z, ZHANG H F, ZHAI M G, et al.Granulite facies metamorphism and crust melting in the Huai’an terrane at-1.95 Ga, North China Craton:new constraints from geology, zircon U-Pb, Lu-Hf isotope and metamorphic conditions of granulites[J].Precambrian Research,2016, 286:126-151.

    [122]

    MA S T, LI X P, LIU H, et al.Ultrahigh Temperature Metamorphic Record of Pelitic Granulites in the Huangtuyao Area of the Huai’an Complex, North China Craton[J].Journal of Earth Science, 2019, 30(6):1178-1196.

    [123]

    张家辉,王惠初, 郭敬辉, 等.天镇-怀安地区变质基性岩墙群:华北克拉通古元古代末期碰撞-伸展构造体制转换标志[J].地球科学, 2020, 45(9):3239-3257.

    [124]

    王洛娟,郭敬辉,彭澎,等.华北克拉通孔兹岩带东端孤山剖面石榴石基性麻粒岩的变质作用及年代学研究[J].岩石学报,2011,27(12):3689-3700.

    [125]

    ZHANG D D, GUO J H, TIAN Z H, et al.Metamorphism and P-T evolution of high pressure granulite in Chicheng, northern part of the Paleoproterozoic Trans-North China Orogen[J].Precambrian Research,2016, 280:76-94.

    [126]

    ZHANG H F, WANG H Z, SANTOSH M, et al.Zircon UPb ages of Paleoproterozoic mafic granulites from the Huai’an terrane, North China Craton(NCC):Implications for timing of cratonization and crustal evolution history[J].Precambrian Research,2016, 272:244-263.

    [127]

    QIAN J H, WEI C J.P-T-t evolution of garnet amphibolites in the Wutai-Hengshan area, North China Craton:insights from phase equilibria and geochronology[J].Journal of Metamorphic Geology, 2016, 34(5):423-446.

    [128]

    WU J L, ZHANG H F, ZHAI M G, et al.Discovery of pelitic high-pressure granulite from Manjinggou of the Huai’an Complex, North China Craton:Metamorphic P-T evolution and geological implications[J].Precambrian Research,2016, 278:323-336.

    [129]

    WU J L, ZHANG H F, ZHAI M G, et al.Paleoproterozoic high-pressure-high-temperature pelitic granulites from Datong in the North China Craton and their geological implications:Constraints from petrology and phase equilibrium modeling[J].Precambrian Research,2017, 303:727-748.

    [130]

    LIU H, LI X P, KONG F M, et al.Ultra-high temperature overprinting of high pressure pelitic granulites in the Huai'an complex, North China Craton:Evidence from thermodynamic modeling and isotope geochronology[J].Gondwana Research, 2019, 72:15-33.

    [121]

    LIU F, GUO J H, PENG P, et al.Zircon U-Pb ages and geochemistry of the Huai’an TTG gneisses terrane:Petrogenesis and implications for-2.5Ga crustal growth in the North China Craton[J].Precambrian Research, 2012, 212-213:225-244.

    [132]

    WANG J, WU Y B, GAO S, et al.Zircon U-Pb and trace element data from rocks of the Huai’an Complex:New insights into the late Paleoproterozoic collision between the Eastern and Western Blocks of the North China Craton[J].Precambrian Research,2010, 178(1-4):59-71.

    [133]

    CAWOOD P A, HAWKESWORTH C J, DHUIME B.Detrital Zircon Record and Tectonic Setting[J].Geology, 2012, 40(10):875-878.

    [134]

    CONDIE K C, BORYTA M D, LIU J Z, et al.The Origin of khondalites, geochemical evidence from the Archean to Early Proterozoic granulite belt in the North China craton[J].Precambrían Research, 1992, 59:207-223.

    [135]

    YIN C Q, ZHAO G C, GUO J H, et al.U-Pband Hf isotopic study of zircons of the Helanshan Complex:constrains on theevolution of the Khondalite Belt in the Western Block of the North China Craton[J].Lithos, 2011, 122, 25-38.

    [136]

    DAN W, LI X H, GUO J H, et al.Integrated in situ zircon U-Pb ageand Hf-O isotopes for the Helanshan khondalites in North China Craton:juvenilecrustal materials deposited in active or passive continental margin[J].Precambrian Research, 2012, 222-223:143-158.

    [137]

    董春艳,刘敦一,万渝生,等.内蒙古大青山地区早前寒武纪变质岩的锆石Hf同位素组成和稀土模式[J].地质论评, 2009,55(04):509-520.

    [138]

    WAN Y S, PENG P, LIU S J, et al.Late Paleoproterozoic tectono-thermal event in the northwestern North China Craton:Evidence from U-Pb dating and O-Hf isotopic compositions of zircons from metasedimentary rocks north of Hohhot City, Inner Mongolia, northern China[J].Journal of Asian Earth Sciences,2018, 167:152-164.

    [139]

    XIA X, SUN M, ZHAO G, et al.U-Pb and Hf isotopic study of detrital zircons from the Lüliang khondalite, North China Craton, and their tectonic implications[J].Geological Magazine,2009, 146(5):701-716.

    [140]

    LIU C H, ZHAO G C, LIU F L, et al.Zircon U-Pb and Lu-Hf isotopic and whole-rock geochemical constraints on the Lanhe and Heichashan Groups:Implications for the Paleoproterozoic tectonic basin evolution of the Lüliang Complex[J].Lithos, 2016, 262:526-545.

    [141]

    LIU C H, ZHAO G C, LIU F L, ET AL.Coexistence of Aand I-type granites in the Lüliang Complex:Tectonic implications for the middle Paleoproterozoic Trans-North China Orogen, North China Craton[J].Lithos,2021, 380-381:105875.

    [142]

    LI S Z, ZHAO G C.SHRIMP U-Pb zircon geochronology of the Liaoji granitoids:constraints on the evolution of the Paleoproterozoic Jiao-Liao-Ji belt in the Eastern Block of the North China Craton[J].Precambrian Research, 2007, 158:1-16.

    [143]

    LI S Z,ZHAO G C,SANTOSH M, et al.Paleoproterozoic structural evolution of the southern segment of the Jiao-Liao-Ji Belt, North China Craton[J].Precambrian Research, 2012, 200-203:59-73.

    [144]

    杜利林,杨崇辉,任留东,等.吕梁地区2.2-2.1Ga岩浆事件及其构造意义[J].岩石学报,2012,28(9):2751-2769.

    [145]

    杜利林,杨崇辉,宋会侠,等.华北克拉通五台地区2.2-2.1Ga花岗岩的成因与构造背景[J].岩石学报,2018,34(4):1154-1174.

    [146]

    DU L L, YANG C H, WANG W, et al.Paleoproterozoic rifting of the North China Craton:geochemical and zircon Hf isotopic evidence from 2137 Ma Huangjinshan A-type granite porphyry in the Wutai area[J].Journal of Asian Earth Sciences, 2013, 72:190-202.

    [147]

    WANG X, ZHU WB, GE RF, et al.Two episodes of Paleoproterozoic metamorphosed mafic dykes in the Lvliang Complex:Implications for the evolution of the Trans-North China Orogen[J].Precambrian Research, 2014, 243:133-148.

    [148]

    PENG P.Precambrian mafic dykes warms in the North China Craton and their geological implications[J].Science China(Earth Sciences), 2015, 58(5):649-675.

    [149]

    董春艳,马铭株,刘守偈,等.华北克拉通古元古代中期伸展体制新证据:鞍山-弓长岭地区变质辉长岩的锆石SHRIMP U-Pb定年和全岩地球化学[J].岩石学报,2012,28(9):2785-2792.

    [150]

    WANG XP, PENG P, WANG C, et al.Nature of three episodes of Paleoproterozoic magmatism(2180 Ma, 2115 Ma and 1890 Ma)in the Liaoji belt, North China with implications for tectonic evolution[J].Precambrian Research, 2017, 298, 252-267.

    [151]

    王惠初,康健丽,任云伟,等.胶-辽-吉带构造属性与演化阶段新划分:胶北变质辉长岩的启示[J].岩石学报,2021,37(1):185-210.

    [152]

    陈海东,黎娇,景耀祖,等.内蒙古中部凉城地区紫苏斜长麻粒岩锆石U-Pb年龄及地质意义[J].中国地质,2014,41(04):1136-1142.

    [153]

    ARTEMIEVA I M, MOONEY W D.Thermal thickness and evolution of Precambrian lithosphere; a global study[J].Journal of Geophysical Research:Solid Earth, 2001, 106(B8):16387-16414.

    [154]

    MOORES E M.Pre-1 Ga(pre-Rodinian)ophiolites:Their tectonic and environmental implications[J].Geological Society of America Bulletin, 2002, 114(1):80-95.

    [155]

    ZHENG Y, ZHAO G.Two styles of plate tectonics in Earth's history[J].Science Bulletin, 2020, 65(4):329-334.

    [156]

    GERYA T.Precambrian geodynamics:Concepts and models[J].Gondwana Research, 2014, 25(2):442-463.

    [157]

    翟明国.华北克拉通的形成以及早期板块构造[J].地质学报,2012,6(09):1335-1349.

    [158]

    SCOTT D J, HELMSTAEDT H, BICKLE M J.Purtuniq ophiolite, Cape Smith belt, northern Quebec, Canada:A reconstructed section of Early Proterozoic oceanic crust[J].Geology, 1992, 20(2):173-176.

    [159]

    PELTONEN P, KONTINEN A, HUHMA H.Petrology and Geochemistry of Metabasalts from the 1.95 Ga Jormua Ophiolite, Northeastern Finland[J].Journal of Petrology, 1996, 37(6):1359-1383.

    [160]

    PELTONEN P AND KONTINEN A.The Jormua Ophiolite:A mafic-ultramafic complex from an ancient ocean-continent transition zone[J].Developments in Precambrian Geology,2004, 13:35-71.

    [161]

    FURNES H, DE WIT M, STAUDIGEL H, et al.A Vestige of Earth's Oldest Ophiolite[J].Science, 2007, 315(5819):1704-1707.

    [162]

    HAMILTON W B.Earth’s First Two Billion Years-the Era of Internally Mobile Crust[J].In:Geological Society of America, Memoir, 2007, 233-296.

    [163]

    KUSKY T M, LI J H, TUCKER R D.The Archean Dongwanzi Ophiolite Complex, North China Craton:2.505-Billion-Year-Old Oceanic Crust and Mantle[J].Science, 2001, 292(5519):1142-1145.

    [164]

    LI J H, KUSKY T M, HUANG X.Neoarchean podiform chromitites and harzburgite tectonite in ophiolitic melange, North China Craton, Remnants of Archean oceanic mantle[J].GSA Today, 2002, 12(7):4-11.

    [165]

    ZHAI M G, ZHAO G C, ZHANG Q, et al.Is the Dongwanzi complex an Archean ophiolite[J].Science, 2002, 295(5557):92.

    [166]

    ZHAO G C, WILDE S A, LI S Z, et al.U-Pb zircon age constraints on the Dongwanzi ultramafic-mafic body, North China, confirm it is not an Archean ophiolite[J].Earth and Planetary Science Letters, 2007, 255(1-2):85-93.

    [167]

    李继亮,王凯怡,王清晨,等.五台山早元古代碰撞造山带初步认识[J].地质科学,1990,25(1):1-11.

    [168]

    王凯怡,李继亮,郝杰,等.山西省五台山晚太古代镁铁质-超镁铁质岩:一种可能的古蛇绿混杂岩[J].岩石学报,1997,13(2):139-151.

    [169]

    KUSKY T M, LI J H, GLASS A AND HUANG X N.Origin and emplacement of Archean ophiolites of the Central Orogenic belt, North China craton.In:Kusky TM(ed.).Precambrian Ophiolites and Related rocks[M].Amsterdam:Elsevier,Developments in Precambrian Geology, 2004, 13:223-274.

    [170]

    POLAT A, KUSKY T M, LI J H, et al.Geochemistry of Neoarchean(ca.2.55-2.50Ga)volcanic and ophiolitic rocks in the Wutaishan greenstone belt central orogenic belt North China Craton:Implications for geodynamic setting and continental growth[J].Geological Society of America Bulletin, 2005, 117:1387-1399.

    [171]

    王仁民,董卫东.冀西北高压麻粒岩带构造环境的再思考[J].地学前缘,1999, 6(4):347-351.

    [172]

    LIU H, ZHANG H.Paleoproterozoic ophiolite remnants in the northern margin of the North China Craton:Evidence from the Chicheng peridotite massif[J].Lithos,2019, 344-345:311-323.

    [173]

    倪志耀,翟明国,王仁民,等.华北古陆块北缘中段发现晚古生代退变榴辉岩[J].科学通报,2004,49(6):585-591.

    [174]

    YANG F, KIM S W, TSUNOGAE T, et al.Multiple enrichment of subcontinental lithospheric mantle with Archean to Mesozoic components:Evidence from the Chicheng ultramafic complex, North China Craton[J].Gondwana Research, 2021, 94:201-221.

    [175]

    CONDIE K C, O’NEILL C, ASTER R C.Evidence and implications for a widespread magmatic shutdown for 250 My on Earth[J].Earth Planet Sci Lett, 2009,282:294-8.

    [176]

    ERIKSSON P G, CONDIE K C.Cratonic sedimentation regimes in the ca.2450-2000Ma period:Relationship to a possible widespread magmatic slowdown on Earth?[J].Gondwana Research, 2014, 25(1):30-47.

    [177]

    POULTON S W, BEKKER A, CUMMING V M, et al.A 200-million-year delay in permanent atmospheric oxygenation[J].Nature, 2021:1-5.

    [178]

    KUSKY T M, WINDLEY B F, SAFONOVA I, et al.Recognition of ocean plate stratigraphy in accretionary orogens through Earth history:A record of 3.8billion years of sea floor spreading, subduction, and accretion[J].Gondwana Research,2013, 24(2):501-547.

    [179]

    ZHAI M, PENG P.Origin of early continents and beginning of plate tectonics[J].Science Bulletin, 2020, 65(12):970-973.

    [180]

    翟明国,张艳斌,李秋立,等.克拉通、下地壳与大陆岩石圈-庆贺沈其韩先生百年华诞[J].岩石学报,2021,37(1):1-23.

    [181]

    BUROV E, GERYA T.Asymmetric three-dimensional topography over mantle plumes[J].Nature, 2014, 513(7516):85-89.

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  23
  • PDF下载数:  4
  • 施引文献:  0
出版历程
收稿日期:  2022-03-07

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回