期刊网首页  /  联系我们  /  English
高级检索
{{news.title}}

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

,  ,  , 

downloadPDF
文章导航 > 岩石学报 > 2016 > 32(3): 713-726

上一篇

下一篇

钟焱, 陈雅丽, 翟明国, 马旭东. 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.
引用本文: 钟焱, 陈雅丽, 翟明国, 马旭东. 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.
shu
ZHONG Yan, CHEN YaLi, ZHAI MingGuo, MA XuDong. Stratigraphic correlation and lithofacies paleogeography of khondalite series in the western North China Craton.[J]. Acta Petrologica Sinica, 2016, 32(3): 713-726.
Citation: ZHONG Yan, CHEN YaLi, ZHAI MingGuo, MA XuDong. Stratigraphic correlation and lithofacies paleogeography of khondalite series in the western North China Craton.[J]. Acta Petrologica Sinica, 2016, 32(3): 713-726.
shu

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

    • 1.

      中国地质调查局天津地质调查中心, 天津 300170

    • 2.

      中国科学院地质与地球物理研究所, 北京 100029

    • 3.

      中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室, 北京 100037

  • 基金项目:

    本文受科技部"973"项目(2012CB4166006)、国家自然科学基金项目(41530208、41210003)和中国地质调查局项目(12120114021701)联合资助.

Stratigraphic correlation and lithofacies paleogeography of khondalite series in the western North China Craton.

    • 1.

      Tianjin Center, China Geological Survey, Tianjin 300170, China

    • 2.

      Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

    • 3.

      MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

    摘要
  • 位于华北克拉通西部的孔兹岩系是探讨华北克拉通形成及演化过程的关键对象之一,近年来的研究显示这套富铝质沉积岩系在1.95~1.82Ga期间经历了高压/高温和超高温-高温/中(低)压两期变质作用。已发表的钻井资料表明鄂尔多斯中、新生代盆地的基底岩石在源区特征、沉积时代、岩石矿物组合和变质时代等方面均与孔兹岩系十分类似,暗示孔兹岩系的原岩分布和后期的高级变质作用范围可能涉及到了鄂尔多斯地块内部。然而,目前对于孔兹岩系的原岩分布、等时性和沉积环境等问题仍有争议,这些问题对于约束孔兹岩系的时空分布和理解华北克拉通西部地区的构造演化过程具有十分重要的科学意义。基于地层学角度的尝试,本文选取贺兰山、大青山和集宁地区的孔兹岩系进行了沉积层序的划分及对比,并初步恢复了相应时期鄂尔多斯地块的岩相古地理特征。本文的研究结果表明:(1)鄂尔多斯地块北缘的贺兰山、大青山和集宁等地区的孔兹岩系均由可对比的三个沉积层序组成;(2)这套沉积岩系的分布范围呈面状延伸至鄂尔多斯地块内部,指示华北克拉通西部曾存在一个克拉通内盆地性质的"鄂尔多斯陆表海",其海侵方向可能由贺兰山-鄂尔多斯地块内部指向大青山、集宁等地区;(3)鄂尔多斯陆表海可能发育于2.5~2.3Ga"构造寂静期"的某一阶段,此间堆积的孔兹岩系(丰镇群)原岩很可能是代表华北陆块完成克拉通化过程的标志性盖层。
    The khondalite series, located in the western part of the North China Craton(NCC), is one of the most significant objects that are essential for understanding formation and evolution of the NCC. To date, a great number of researches suggested that the khondalite series, a suite of high-grade metamorphic alumina-rich sedimentary rocks, had witnessed two important metamorphic events during 1.95~1.82Ga, including high pressure/high temperature metamorphism and high to unltra-high temperature/medium to low pressure metamorphism. The available data from drilling samples of the Mesozoic-Cenozoic Ordos Basin revealed that its basement rocks were similar with the khondalite series in petrology, provenance, depositional age and metamorphic timing. It appears that a larger part of the Ordos Block had been covered by the protolithes of the khondalite series and been involved by the subsequent high-grade metamorphic events. However, the debates on the distribution, isochronism and depositional environment of the protolithes of the khondalite series are still ongoing. These points are invaluable for constraining temporal-spatial distribution of the khondalite series and understanding tectonic evolution of the western NCC. As an attempt to facilitate deciphering the protolith basin, three typical sections of the khondalite series in the Helanshan, Daqingshan and Jining areas were chosen for deposition sequence subdivisions, stratigraphic correlation and lithofacies paleogeographic rebuilding. These results in this paper suggest that:(1) the khondalite series in the northern margin of the Ordos Block are composed of three correlatable deposition sequences;(2) an epeiric sea over the Ordos Block(Ordos Epeiric Sea) might be responsible for the planar distribution of the khondalite series and its transgressive direction was mainly from the Helanshan-interior of the block to the Daqingshan and Jining areas; and(3) the Ordos Epeiric Sea induced accumulation was completed during the inactive period(2.5~2.3Ga) and the khondalite series might be the first sedimentary cover after the cratonization of the NCC.
    • HTML全文
  • 加载中
    • 参考文献(110)
  • [1]

    Bureau of Geology and Mineral Resources of Nei Mongol Autonomous Region. 1991. Regional geology of Nei Mongol(Inner Mongolia) Autonomous Region. Beijing:Geological Publishing House, 9-31(in Chinese)

    [2]

    Bureau of Geology and Mineral Resources of Nei Mogol Autonomous Region. 1996. Stratigraphy(Lithostratic) of Nei Mongol Autonomous Region. In:Li W(ed.). Multiple Classification and Correlation of the Stratigraphy of China. Wuhan:China University of Geosciences Press, 114-120(in Chinese)

    [3]

    Bureau of Geology and Mineral Resources of Ningxia Hui Autonomous Region. 1990. Regional Geology of Ningxia Hui Autonomous Region. Beijing:Geological Publishing House, 7-25(in Chinese)

    [4]

    Cai J, Liu PH, Liu FL, Liu JH, Wang F and Shi JR. 2013. Genetic mineralogy and metamorphic evolution of Al-rich gneisses in the Shiguai area, Daqingshan-Wulashan metamorphic complex belt. Acta Petrologica Sinica, 29(2):437-461(in Chinese with English abstract)

    [5]

    Cai J, Liu FL, Liu PH, Liu CH, Wang F and Shi JR. 2014. Metamorphic P-T path and tectonic implications of pelitic granulites from the Daqingshan Complex of the Khondalite Belt, North China Craton. Precambrian Research, 241:161-184

    [6]

    Cai J, Liu FL, Liu PH and Shi JR. 2014. Metamorphic P-T conditions and U-Pb dating of the sillimanite-cordierite-garnet paragneisses in Sanchakou, Jining area, Inner Mongolia. Acta Petrologica Sinica, 30(2):472-490(in Chinese with English abstract)

    [7]

    Condie KC, Boryta MD, Liu JZ and Qian XL. 1992. The origin of khondalites:Geochemical evidence from the Archean to Early Proterozoic granulite belt in the North China craton. Precambrian Research, 59(3-4):207-223

    [8]

    Dan W, Li XH, Guo JH, Liu Y and Wang XC. 2012. Integrated in situ zircon U-Pb age and Hf-O isotopes for the Helanshan khondalites in North China Craton:Juvenile crustal materials deposited in active or passive continental margin? Precambrian Research, 222-223:143-158

    [9]

    Dan W, Li XH, Wang Q, Wang XC, Liu Y and Wyman DA. 2014. Paleoproterozoic S-type granites in the Helanshan Complex, Khondalite Belt, North China Craton:Implications for rapid sediment recycling during slab break-off. Precambrian Research, 254:59-72

    [10]

    Dong CY, Liu DY, Li JJ, Wan YS, Zhou HY, Li CD, Yang YH and Xie LW. 2007. Palaeoproterozoic Khondalite Belt in the western North China Craton:New evidence from SHRIMP dating and Hf isotope composition of zircons from metamorphic rocks in the Bayan Ul-Helan Mountains area. Chinese Science Bulletin, 52(21):2984-2994

    [11]

    Dong CY, Wan YS, Xu ZY, Liu DY, Yang ZS, Ma MZ and Xie HQ. 2013. SHRIMP zircon U-Pb dating of Late Paleoproterozoic kondalites in the Daqing Mountains area on the North China Craton. Science China(Earth Sciences), 56(1):115-125

    [12]

    Dong CY, Wan YS, Wilde SA, Xu ZY, Ma MZ, Xie HQ and Liu DY. 2014. Earliest Paleoproterozoic supracrustal rocks in the North China Craton recognized from the Daqingshan area of the Khondalite Belt:Constraints on craton evolution. Gondwana Research, 25(4):1535-1553

    [13]

    Dong QX and Zhou JC. 1984. Stratigraphic division of the original Wulashan Group in the Wula Mountains, Nei Monggol(Inner Mongolia). Regional Geology of China,(3):19-37(in Chinese with English abstract)

    [14]

    Gou LL, Zhang CL and Wang Q. 2015. Petrological evidence for isobaric cooling of ultrahightemperature pelitic granulites from the Khondalite Belt, North China Craton. Science Bulletin, 60(17):1535-1542

    [15]

    Guo JH, Chen Y, Peng P, Liu F, Chen L and Zhang LQ. 2006. Sapphirine granulite from Daqingshan area, Inner Mongolia~1.85Ga ultrahigh temperature(UHT) metamorphism. In:2006's National Symposium on Petrology and Geodynamics. Nanjing:Nanjing University, 213-216(in Chinese)

    [16]

    Guo JH, Peng P, Chen Y, Jiao SJ and Windley BF. 2012. UHT sapphirine granulite metamorphism at 1.93~1.92Ga caused by gabbronorite intrusions:Implications for tectonic evolution of the northern margin of the North China Craton. Precambrian Research, 222-223:124-142

    [17]

    Hu JM, Liu XS, Li ZH, Zhao Y, Zhang SH, Liu XC, Qu HJ and Chen H. 2013. SHRIMP U-Pb zircon dating of the Ordos Basin basement and its tectonic significance. Chinese Science Bulletin, 58(1):118-127

    [18]

    Huo FC, Cao JX, Dong YS, Gu QC and Yan ZQ. 1987. The division, correlation, metamorphism and mineralization features of the lower and middle Precambrian in the Helanshan Mountain-Alashan region, China. Journal of Changchun College of Geology, 17(1):35-46(in Chinese with English abstract)

    [19]

    Kusky TM and Li JH. 2003. Paleoproterozoic tectonic evolution of the North China Craton. Journal of Asian Earth Sciences, 22(4):383-397

    [20]

    Kusky T, Li JH and Santosh M. 2007. The Paleoproterozoic North Hebei Orogen:North China craton's collisional suture with the Columbia supercontinent. Gondwana Research, 12(1-2):4-28

    [21]

    Kusky TM. 2011. Geophysical and geological tests of tectonic models of the North China Craton. Gondwana Research, 20(1):26-35

    [22]

    Li JH, Qian XL and Liu SW. 2000. Geochemistry of khondalites from the central portion of North China craton(NCC):Implications for the continental cratonization in the Neoarchean. Science in China(Series D), 43(3):253-265

    [23]

    Li JH, Qian XL, Huang XN and Liu SW. 2000. Tectonic framework of North China Block and its cratonization in the Early Precambrian. Acta Petrologica Sinica, 16(1):1-10(in Chinese with English abstract)

    [24]

    Li LM, Zeng ZX, Lu YJ, Wei YX, Xiang SM and Pan LL. 2014. LA-ICP-MS U-Pb geochronology of detrital zircons from the Zhaochigou Formation-complex in the Helan Mountain and its tectonic significance. Chinese Science Bulletin, 59(13):1425-1437

    [25]

    Li XP, Yang ZY, Zhao GC, Grapes R and Guo JH. 2011. Geochronology of khondalite-series rocks of the Jining Complex:Confirmation of depositional age and tectonometamorphic evolution of the North China Craton. International Geology Review, 53(10):1194-1211

    [26]

    Liu JH, Liu FL, Ding ZJ, Chen JQ, Liu PH, Shi JR, Cai J and Wang F. 2013. Zircon U-Pb chronology, geochemistry and their petrogenesis of Early Paleoproterozoic granitoid gneisses in Ulashan area, North China Craton. Acta Petrologica Sinica, 29(2):485-500(in Chinese with English abstract)

    [27]

    Liu PH, Liu FL, Cai J, Liu JH, Shi JR and Wang F. 2013. Geochronological and geochemical study of the Lijiazi mafic granulites from the Daqingshan-Wulashan metamorphic complex, the central Khondalite Belt in the North China Craton. Acta Petrologica Sinica, 29(2):462-484(in Chinese with English abstract)

    [28]

    Lu LZ, Xu XC and Liu FL. 1996. Early Precambrian Khondalite Series in Northern China. Changchun:Changchun Publishing House, 1-125(in Chinese)

    [29]

    Ma MZ, Dong CY, Xu ZY, Xie SW, Liu DY and Wan YS. 2015. Anatexis of Early Paleoproterozoic garnet-biotite gneisses(Daqingshan supracrustal rocks) in Daqingshan, Inner Mongolia:Geology, zircon geochronology and geochemistry. Acta Petrologica Sinica, 31(6):1535-1548(in Chinese with English abstract)

    [30]

    Peng P, Zhai MG, Li QL, Wu FY, Hou QL, Li Z, Li TS and Zhang YB. 2011. Neoproterozoic(~900Ma) Sariwon sills in North Korea:Geochronology, geochemistry and implications for the evolution of the south-eastern margin of the North China Craton. Gondwana Research, 20(1):243-254

    [31]

    Peng P, Wang XP, Windley BF, Guo JH, Zhai MG and Li Y. 2014. Spatial distribution of ca.1950~1800Ma metamorphic events in the North China Craton:Implications for tectonic subdivision of the craton. Lithos, 202-203:250-266

    [32]

    Qian XL, Cui WY and Wang SQ. 1985. Evolution of the Inner Mongolia-eastern Hebei Archaean granulite belt in the North China Craton. In:Department of Geology, Peking University(ed.). The Records of Geological Research. Beijing:Beijing University Press, 20-29(in Chinese)

    [33]

    Qian XL and Li JH. 1999. Discovery of Neoarchean unconformity and its implication for continental cratonization of North China Craton. Science in China(Series D), 42(4):399-407

    [34]

    Rogers JJW and Santosh M. 2002. Configuration of Columbia:A Mesoproterozoic supercontinent. Gondwana Research, 5(1):5-22

    [35]

    Rogers JJW and Santosh M. 2009. Tectonics and surface effects of the supercontinent Columbia. Gondwana Research, 15(3-4):373-380

    [36]

    Santosh M, Tsunogae T, Li JH and Liu SJ. 2007. Discovery of sapphirine-bearing Mg-Al granulites in the North China Craton:Implications for Paleoproterozoic ultrahigh temperature metamorphism. Gondwana Research, 11(3):263-285

    [37]

    Santosh M, Sajeev K, Li JH, Liu SJ and Itaya T. 2009. Counterclockwise exhumation of a hot orogen:The Paleoproterozoic ultrahigh-temperature granulites in the North China Craton. Lithos, 110(1-4):140-152

    [38]

    Wan YS, Song B, Liu DY, Wilde SA, Wu JS, Shi YR, Yin XY and Zhou HY. 2006. SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary rocks in the North China Craton:Evidence for a major Late Palaeoproterozoic tectonothermal event. Precambrian Research, 149(3-4):249-271

    [39]

    Wan YS, Liu DY, Dong CY, Xu ZY, Wang ZJ, Wilde SA, Yang YH, Liu ZH and Zhou HY. 2009. The Precambrian Khondalite Belt in the Daqingshan area, North China Craton:Evidence for multiple metamorphic events in the Palaeoproterozoic era. Geological Society, London, Special Publications, 323(1):73-97

    [40]

    Wan YS, Xu ZY, Dong CY, Nutman A, Ma MZ, Xie HQ, Liu SJ, Liu DY, Wang HC and Gu H. 2013a. Episodic Paleoproterozoic(~2.45,~1.95 and ~1.85Ga) mafic magmatism and associated high temperature metamorphism in the Daqingshan area, North China Craton:SHRIMP zircon U-Pb dating and whole-rock geochemistry. Precambrian Research, 224:71-93

    [41]

    Wan YS, Xie HQ, Yang H, Wang ZJ, Liu DY, Kröner A, Wilde SA, Geng YS, Sun LY, Ma MZ, Liu SJ, Dong CY and Du LL. 2013b. Is the Ordos Block Archean or Paleoproterozoic in age? Implications for the Precambrian evolution of the North China Craton. American Journal of Science, 313(7):683-711

    [42]

    Wang LJ, Guo JH, Peng P and Liu F. 2011. Metamorphic and geochronological study of garnet-bearing basic granulites from Gushan, the eastern end of the Khondalite Belt in the North China Craton. Acta Petrologica Sinica, 27(12):3689-3700(in Chinese with English abstract)

    [43]

    Wang W, Liu XS, Hu JM, Li ZH, Zhao Y, Zhai MG, Liu XC, Clarke G, Zhang SH and Qu HJ. 2014. 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. Precambrian Research, 251:181-196

    [44]

    Wu CH, Zhong CT and Chen QA. 1997. Discussion on the age of Khondalite in Jin-Meng(Shanxi-Nei Mongol) high-grade terrain. Acta Petrologica Sinica, 13(3):289-302(in Chinese with English abstract)

    [45]

    Wu CH and Zhong CT. 1998. Early Proterozoic SW-NE collision model for the central part of the North China Craton:Implications for tectonic regime of the Khondalite downward into lower crust in Jin-Meng high-grade region. Progress in Precambrian Research, 21(3):28-50(in Chinese with English abstract)

    [46]

    Wu CH, Sun M, Li HM, Zhao GC and Xia XP. 2006. LA-ICP-MS U-Pb zircon ages of the khondalites from the Wulashan and Jining high-grade terrain in northern margin of the North China Craton:Constraints on sedimentary age of the khondalite. Acta Petrologica Sinica, 22(11):2639-2654(in Chinese with English abstract)

    [47]

    Wu CH. 2007. Meta-sedimentary rocks and tectonic division of the North China Craton. Geological Journal of China Universities, 13(3):442-457(in Chinese with English abstract)

    [48]

    Xia XP, Sun M, Zhao GC and Luo Y. 2006a. LA-ICP-MS U-Pb geochronology of detrital zircons from the Jining Complex, North China Craton and its tectonic significance. Precambrian Research, 144(3-4):199-212

    [49]

    Xia XP, Sun M, Zhao GC, Wu FY, Xu P, Zhang JH and Luo Y. 2006b. U-Pb and Hf isotopic study of detrital zircons from the Wulashan khondalites:Constraints on the evolution of the Ordos Terrane, Western Block of the North China Craton. Earth and Planetary Science Letters, 241(3-4):581-593

    [50]

    Xiao PX, You WF, Xie CR, Li P and Bai SM. 2011. LA-ICP-MS U-Pb detrital zircon geochronology of alumina-rich gneiss of the Helanshan complex-group in the northern segment of Helanshan Mountains and regional comparison. Geological Bulletin of China, 30(1):26-36(in Chinese with English abstract)

    [51]

    Xu ZY, Liu ZH and Yang ZS. 2002. The strata texture of khondalite in Daqingshan area, Inner Mongolia. Journal of Jilin University(Earth Science Edition), 32(4):313-318(in Chinese with English abstract)

    [52]

    Xu ZY, Liu ZH, Hu FX and Yang ZS. 2005. Geochemical characteristics of the calc-silicate rocks in Khondalite Series in Daqingshan area, Inner Mongolia. Journal of Jilin University(Earth Science Edition), 35(6):681-689(in Chinese with English abstract)

    [53]

    Xu ZY, Liu ZH, Dong XJ, Dong CY and Wan YS. 2011. Discovery of kyanite garnet quartzfeldspathic gneiss in the north side of Daqing Mts., Inner Mongolia, and its petrography, geochemistry and zircon SHRIMP dating. Geological Review, 57(2):243-252(in Chinese with English abstract)

    [54]

    Xu ZY, Fan ZW, Liu ZH, Li SC, Wang WQ, Zhang C, Ma Y and Wang YN. 2013. Formation age of the marble in the khondalite series in Jining, Inner Mongolia:Evidence of the LA-ICP-MS zircon U-Pb dating of felsic gneiss. Journal of Jilin University(Earth Science Edition), 43(3):809-819(in Chinese with English abstract)

    [55]

    Yang QY, Santosh M and Wada H. 2014. Graphite mineralization in Paleoproterozoic khondalites of the North China Craton:A carbon isotope study. Precambrian Research, 255:641-652

    [56]

    Yang ZS, Xu ZY and Liu ZH. 2000. Khondalite event and Archean crust structure evolvement. Progress in Precambrian Research, 23(4):206-212(in Chinese with English abstract)

    [57]

    Yang ZS, Xu ZY, Liu ZH and Peng XD. 2003. Consideration and practice of the construction of litho stratigraphic systems in high-grade metamorphic terrains:A case study in the Daqingshan-Wulashan area. Geology in China, 30(4):343-351(in Chinese with English abstract)

    [58]

    Yin CQ, Zhao GC, Sun M, Xia XP, Wei CJ, Zhou XW and Leung WH. 2009. LA-ICP-MS U-Pb zircon ages of the Qianlishan Complex:Constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton. Precambrian Research, 174(1-2):78-94

    [59]

    Yin CQ, Zhao GC, Guo JH, Sun M, Xia XP, Zhou XW and Liu CH. 2011. 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. Lithos, 122(1-2):25-38

    [60]

    Zhai MG and Liu WJ. 2003. Palaeoproterozoic tectonic history of the North China craton:A review. Precambrian Research, 122(1-4):183-199

    [61]

    Zhai MG. 2004. 2.1~1.7Ga geological event group and its geotectonic significance. Acta Petrologica Sinica, 20(6):1343-1354(in Chinese with English abstract)

    [62]

    Zhai MG, Guo JH and Liu WJ. 2005. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton:A review. Journal of Asian Earth Sciences, 24(5):547-561

    [63]

    Zhai MG and Peng P. 2007. Paleoproterozoic events in the North China Craton. Acta Petrologica Sinica, 23(11):2665-2682(in Chinese with English abstract)

    [64]

    Zhai MG. 2009. Two kinds of granulites(HT-HP and HT-UHT) in North China Craton:Their genetic relation and geotectonic implications. Acta Petrologica Sinica, 25(8):1753-1771(in Chinese with English abstract)

    [65]

    Zhai MG. 2011. Cratonization and the Ancient North China Continent:A summary and review. Science China(Earth Sciences), 54(8):1110-1120

    [66]

    Zhai MG and Santosh M. 2011. The Early Precambrian odyssey of the North China Craton:A synoptic overview. Gondwana Research, 20(1):6-25

    [67]

    Zhai MG. 2013. Secular changes of metallogenic systems link with continental evolving of the North China Craton. Acta Petrologica Sinica, 29(5):1759-1773(in Chinese with English abstract)

    [68]

    Zhang CL, Diwu CR, Kröner A, Sun Y, Luo JL, Li QL, Gou LL, Lin HB, Wei XS and Zhao J. 2015. 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. Precambrian Research, 267:121-136

    [69]

    Zhang HF, Zhai MG, Santosh M, Wang HZ, Zhao L and Ni ZY. 2014. 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. Ore Geology Reviews, 63:478-497

    [70]

    Zhao GC, Cawood PA, Wilde SA and Sun M. 2002. Review of global 2.1~1.8Ga orogens:Implications for a pre-Rodinia supercontinent. Earth-Science Reviews, 59(1-4):125-162

    [71]

    Zhao GC, Sun M, Wilde SA and Li SZ. 2003. Assembly, accretion and breakup of the Paleo-Mesoproterozoic Columbia supercontinent:Records in the North China Craton. Gondwana Research, 6(3):417-434

    [72]

    Zhao GC, Sun M, Wilde SA and Li SZ. 2004. A Paleo-Mesoproterozoic supercontinent:Assembly, growth and breakup. Earth-Science Reviews, 67(1-2):91-123

    [73]

    Zhao GC, Sun M, Wilde SA and Li SZ. 2005. Late Archean to Paleoproterozoic evolution of the North China Craton:Key issues revisited. Precambrian Research, 136(2):177-202

    [74]

    Zhao GC and Cawood PA. 2012. Precambrian geology of China. Precambrian Research, 222-223:13-54

    [75]

    Zhao GC, Cawood PA, Li SZ, Wilde SA, Sun M, Zhang J, He YH and Yin CQ. 2012. Amalgamation of the North China Craton:Key issues and discussion. Precambrian Research, 222-223:55-76

    [76]

    Zhou XW and Geng YS. 2009. Metamorphic age of the khondalite series in the Helanshan region:Constraints on the evolution of the Western Block in the North China Craton. Acta Petrologica Sinica, 25(5):1843-1852(in Chinese with English abstract)

    [77]

    Zhou XW, Zhao GC and Geng YS. 2010. Helanshan high pressure pelitic granulite:Petrologic evidence for collision event in the western block of the North China Craton. Acta Petrologica Sinica, 26(7):2113-2121(in Chinese with English abstract)

    [78]

    蔡佳, 刘平华, 刘福来, 刘建辉, 王舫, 施建荣. 2013. 大青山-乌拉山变质杂岩带石拐地区富铝片麻岩成因矿物学与变质演化. 岩石学报, 29(2):437-461

    [79]

    蔡佳, 刘福来, 刘平华, 施建荣. 2014. 内蒙古集宁三岔口夕线堇青石榴二长片麻岩变质作用及年代学研究. 岩石学报, 30(2):472-490

    [80]

    董启贤, 周俊昌. 1984. 内蒙古乌拉山区原乌拉山群地层划分新议. 中国区域地质,(3):19-37

    [81]

    郭敬辉, 陈意, 彭澎, 刘富, 陈亮, 张履桥. 2006. 内蒙古大青山假蓝宝石麻粒岩——1.85Ga的超高温(UHT)变质作用. 见:2006年全国岩石学与地球动力学研讨会. 南京:南京大学, 213-216

    [82]

    霍福臣, 曹景轩, 董燕生, 顾其昌, 闫志强. 1987. 贺兰山-阿拉善地区下、中前寒武系的划分对比及其变质、成矿作用特征. 长春地质学院学报, 17(1):35-46

    [83]

    李江海, 钱祥麟, 黄雄南, 刘树文. 2000. 华北陆块基底构造格局及早期大陆克拉通化过程. 岩石学报, 16(1):1-10

    [84]

    刘建辉, 刘福来, 丁正江, 陈军强, 刘平华, 施建荣, 蔡佳, 王舫. 2013. 乌拉山地区早古元古代花岗质片麻岩的锆石U-Pb年代学、地球化学及成因. 岩石学报, 29(2):485-500

    [85]

    刘平华, 刘福来, 蔡佳, 刘建辉, 施建荣, 王舫. 2013. 华北克拉通孔兹岩带中段大青山-乌拉山变质杂岩立甲子基性麻粒岩年代学及地球化学研究. 岩石学报, 29(2):462-484

    [86]

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

    [87]

    马铭株, 董春艳, 徐仲元, 谢士稳, 刘敦一, 万渝生. 2015. 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. 岩石学报, 31(6):1535-1548

    [88]

    内蒙古自治区地质矿产局. 1991. 内蒙古自治区区域地质志. 北京:地质出版社, 9-31

    [89]

    内蒙古自治区地质矿产局. 1996. 内蒙古自治区岩石地层. 见:李文国编. 全国地层多重划分对比研究. 武汉:中国地质大学出版社, 114-120

    [90]

    宁夏回族自治区地质矿产局. 1990. 宁夏回族自治区区域地质志. 北京:地质出版社, 7-25

    [91]

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

    [92]

    钱祥麟, 李江海. 1999. 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. 中国科学(D辑), 29(1):1-8

    [93]

    王洛娟, 郭敬辉, 彭澎, 刘富. 2011. 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. 岩石学报, 27(12):3689-3700

    [94]

    吴昌华, 钟长汀, 陈强安. 1997. 晋蒙高级地体孔兹岩系的时代. 岩石学报, 13(3):289-302

    [95]

    吴昌华, 钟长汀. 1998. 华北陆台中段吕梁期的SW-NE向碰撞——晋蒙高级区孔兹岩系进入下地壳的构造机制. 前寒武纪研究进展, 21(3):28-50

    [96]

    吴昌华, 孙敏, 李惠民, 赵国春, 夏小平. 2006. 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. 岩石学报, 22(11):2639-2654

    [97]

    吴昌华. 2007. 华北克拉通的变质沉积岩及其克拉通的构造划分. 高校地质学报, 13(3):442-457

    [98]

    校培喜, 由伟丰, 谢从瑞, 李平, 白生明. 2011. 贺兰山北段贺兰山岩群富铝片麻岩碎屑锆石LA-ICP-MS U-Pb定年及区域对比. 地质通报, 30(1):26-36

    [99]

    徐仲元, 刘正宏, 杨振升. 2002. 内蒙古大青山地区孔兹岩系的地层结构. 吉林大学学报(地球科学版), 32(4):313-318

    [100]

    徐仲元, 刘正宏, 胡凤翔, 杨振升. 2005. 内蒙古大青山地区孔兹岩系中钙硅酸盐岩的组成和地球化学特征. 吉林大学学报(地球科学版), 35(6):681-689

    [101]

    徐仲元, 刘正宏, 董晓杰, 董春艳, 万渝生. 2011. 内蒙古大青山北麓蓝晶石榴长英质片麻岩的发现:岩相学、地球化学和锆石SHRIMP定年. 地质论评, 57(2):243-252

    [102]

    徐仲元, 范志伟, 刘正宏, 李世超, 王挽琼, 张超, 马越, 王英男. 2013. 内蒙集宁地区孔兹岩系中大理岩的形成时代——长英质片麻岩中LA-ICP-MS锆石U-Pb测年的证据. 吉林大学学报(地球科学版), 43(3):809-819

    [103]

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

    [104]

    杨振升, 徐仲元, 刘正宏, 彭向东. 2003. 高级变质区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. 中国地质, 30(4):343-351

    [105]

    翟明国. 2004. 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 20(6):1343-1354

    [106]

    翟明国, 彭澎. 2007. 华北克拉通古元古代构造事件. 岩石学报, 23(11):2665-2682

    [107]

    翟明国. 2009. 华北克拉通两类早前寒武纪麻粒岩(HT-HP和HT-UHT)及其相关问题. 岩石学报, 25(8):1753-1771

    [108]

    翟明国. 2013. 华北前寒武纪成矿系统与重大地质事件的联系. 岩石学报, 29(5):1759-1773

    [109]

    周喜文, 耿元生. 2009. 贺兰山孔兹岩系的变质时代及其对华北克拉通西部陆块演化的制约. 岩石学报, 25(8):1843-1852

    [110]

    周喜文, 赵国春, 耿元生. 2010. 贺兰山高压泥质麻粒岩——华北克拉通西部陆块拼合的岩石学证据. 岩石学报, 26(7):2113-2121

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  5402
  • PDF下载数:  4372
  • 施引文献:  0
出版历程
收稿日期:  2015-01-19
修回日期:  2015-07-30
刊出日期:  2016-03-31

目录

    返回

    地址：北京9825信箱/北京朝阳区北土城西路19号邮编：100029

    电话：(010) 82998205/82998135/82998137 邮箱：ysxb@mail.iggcas.ac.cn

    版权所有 © 2009-2023 岩石学报 京ICP备05029136号-23

    本系统由 北京仁和汇智信息技术有限公司开发