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    华北板块中部晚二叠世-早三叠世砂岩碎屑锆石U-Pb定年及物源判别

    冯志强 刘永江 王权 史建儒 魏荣珠 卫彦升 雷勇

    冯志强, 刘永江, 王权, 史建儒, 魏荣珠, 卫彦升, 雷勇, 2023. 华北板块中部晚二叠世-早三叠世砂岩碎屑锆石U-Pb定年及物源判别. 地球科学, 48(4): 1288-1306. doi: 10.3799/dqkx.2022.071
    引用本文: 冯志强, 刘永江, 王权, 史建儒, 魏荣珠, 卫彦升, 雷勇, 2023. 华北板块中部晚二叠世-早三叠世砂岩碎屑锆石U-Pb定年及物源判别. 地球科学, 48(4): 1288-1306. doi: 10.3799/dqkx.2022.071
    Feng Zhiqiang, Liu Yongjiang, Wang Quan, Shi Jianru, Wei Rongzhu, Wei Yansheng, Lei Yong, 2023. Detrial Zircon U-Pb Dating and Provenance Analysis for Late Permian-Early Triassic Sandstone in Central North China Craton. Earth Science, 48(4): 1288-1306. doi: 10.3799/dqkx.2022.071
    Citation: Feng Zhiqiang, Liu Yongjiang, Wang Quan, Shi Jianru, Wei Rongzhu, Wei Yansheng, Lei Yong, 2023. Detrial Zircon U-Pb Dating and Provenance Analysis for Late Permian-Early Triassic Sandstone in Central North China Craton. Earth Science, 48(4): 1288-1306. doi: 10.3799/dqkx.2022.071

    华北板块中部晚二叠世-早三叠世砂岩碎屑锆石U-Pb定年及物源判别

    doi: 10.3799/dqkx.2022.071
    基金项目: 

    中国地质调查局项目 121201102000150012-05

    中国地质调查局项目 HXCT01-2018F005

    山西省自然科学基金 2019L0126

    山西省自然科学基金 2019L0054

    山西地质博物馆地勘基金18-19年古生物化石调查项目 ZDF03-FC190802

    山西省优秀博士来晋工作奖励基金 SXYBKY2019032

    山西农业大学科技创新基金项目 2020BQ47

    详细信息
      作者简介:

      冯志强(1984-),男,副教授,硕士生导师,主要从事构造地质学方面的研究. ORCID:0000-0002-1197-5749. E-mail:fengzhiqiang@tyut.edu.cn

    • 中图分类号: P548

    Detrial Zircon U-Pb Dating and Provenance Analysis for Late Permian-Early Triassic Sandstone in Central North China Craton

    • 摘要: 华北板块陆内盆地晚二叠世-早三叠世地层沉积物的物源一直存在较大争议.对华北板块中部鄂尔多斯盆地东缘(山西柳林县)上二叠统孙家沟组(2个)和下三叠统刘家沟组(2个)以及沁水盆地(山西沁水县)上二叠统孙家沟组(1个)地层砂岩样品进行了全岩地球化学分析和碎屑锆石LA-MC-ICPMS U-Pb年龄测定.364个单颗粒锆石中,古生代碎屑锆石约占21%,具有~275 Ma(218~333 Ma,65颗)和~431 Ma的两个峰值年龄(368~442 Ma,10颗);前寒武纪碎屑锆石约占79%,具有明显的~1 888 Ma(1 562~2 222 Ma,178颗)和~2 529 Ma(2 253~3 167 Ma,111颗)两个峰值年龄.在前人研究基础上,采用最年轻单颗粒年龄(YSG)和最年轻的碎屑锆石加权平均年龄(TuffZirc)限定地层最大沉积年龄的方法,确定刘家沟组的2个样品沉积下限年龄为253±7 Ma和250±7 Ma,孙家沟组3个样品沉积下限分别为256±7 Ma(MSWD=1.1,n=31)、264±11 Ma(MSWD=4.3,n=7)、250±6 Ma(MSWD=3.6,n=6),与二叠系-三叠系沉积界限年龄251.0±0.4 Ma相接近,其中研究区刘家沟组砂岩的地质时代应归属于早三叠世,孙家沟组砂岩应归属于晚二叠世,并进一步推测华北山西地区孙家沟组沉积时代北部早于南部.根据研究区晚二叠世-早三叠世沉积环境和构造背景分析,以及潜在物源区年龄图谱对比,结合古水流野外分析结果,判别刘家沟组和孙家沟组砂岩中的前寒武纪碎屑锆石物源区为华北板块的变质基底,早古生代碎屑锆石主要来源于兴蒙造山带南缘的早古生代侵入岩,晚古生代碎屑锆石主要来源于内蒙古隆起的晚古生代侵入岩.

       

    • 图  1  华北板块区域地质简图(a)和山西省区域地质图(b)(据Zhao et al., 2005; Meng et al., 2019修改)

      图a中,1.石拐子盆地;2.西山盆地;3.下板城盆地;4.牛营子盆地;5.北票盆地;6.汝箕沟盆地;7.静乐地区;8.济阳地区;9.豫西地区;10.合肥盆地;F1.离石断裂;F2.洪涛山-鹅毛口断裂;F3.狐偃山断裂;F4.太岳山断裂;F5.横河断裂;F6.太行山断裂;F7.系舟山断裂;F8.唐河断裂

      Fig.  1.  Simplified tectonic map showing the North China craton (a) and geological map of the Shanxi Province (b)(modified from Zhao et al., 2005; Meng et al., 2019)

      图  2  研究区石炭系-三叠系地层柱状图

      Fig.  2.  Stratigraphic column for the Carboniferous-Triassic in the study area

      图  3  柳林地区和沁水地区孙家沟组、刘家沟组地层特征

      a.柳林郝家津孙家沟组与刘家沟组接触关系;b~c.刘家沟组灰绿色砂岩,孙家沟组紫红色砂岩;d~e.柳林地区孙家沟组上部晚古生代脊椎动物化石及化石层剖面;f.柳林薛村南刘家沟组和孙家沟组接触关系;g.柳林地区孙家沟组砂岩平行层理;h~i.沁水端氏镇凝灰质长石砂岩野外照片

      Fig.  3.  Sedimentary characteristics of the Sunjiagou and Liujiagou formations in Liulin and Qinshui areas

      图  4  研究区砂岩野外露头及显微特征

      a~b.柳林地区刘家沟组砂岩显微照片;c~d.柳林地区孙家沟组砂岩显微照片;e~f.沁水盆地凝灰质砂岩野外露头和显微照片;Q.石英;Qm.单晶石英;Pl.斜长石;K.钾长石;Lv.火山岩碎屑;Ls.沉积岩碎屑;Lm.变质岩碎屑

      Fig.  4.  Outcrop and microscopic characteristics of the sandstone in studied area

      图  5  研究区孙家沟组与刘家沟组砂岩样品碎屑锆石CL图像

      Fig.  5.  CL images of detrital zircon of sandstone samples from the Sunjiagou and Liujiagou formations

      图  6  研究区刘家沟组与孙家沟组砂岩碎屑锆石U-Pb定年谐和图和频谱图

      Fig.  6.  LA-ICP-MS U-Pb concordia diagrams and histograms of detrital zircon of sandstone samples in Liujiagou and Sunjiagou formations

      图  7  刘家沟组和孙家沟组砂岩稀土元素球粒陨石(a);全球大陆平均上地壳标准化稀土元素配分曲线(b);刘家沟组和孙家沟组砂岩原始地幔标准化微量元素蛛网图(c)

      球粒陨石,全球大陆平均上地壳和原始地幔的标准化数值分别据文献Boynton,1984Sun and McDonough,1989McLennan et al.,1993

      Fig.  7.  Chondrite-normalized REE diagram (a); UCC-normalized REE diagram (b); primitive mantle-normalized trace elements diagram of the Liujiagou and Sunjiagou formations(c)

      图  8  刘家沟组和孙家沟组砂岩Q-F-L和Qm-F-Lt三元图(Dickinson et al.,1983

      Fig.  8.  Tectonic discrimination triangle diagrams of Q-F-L and Qm-F-Lt for the Liujiagou and Sunjiagou formations(Dickinson et al., 1983)

      图  9  研究区孙家沟组地层古水流玫瑰花图

      Fig.  9.  The paleocurrent rose map of the Sunjiagou Formation

      图  10  刘家沟组和孙家沟组砂岩源区母岩性质判别图

      P1.基性火山岩物源区;P2.中性火山岩物源区;P3.酸性火山岩物源区;P4.成熟大陆石英质物源区a. F1’-F2’判别图解(底图据Roser and Korsch,1988);b. K2O-Rb判别图解(据Floyd and Leveridge,1987);c. La/Th-Hf判别图解(据毛光周和刘池洋,2011

      Fig.  10.  Discrimination diagrams of parent rocks for the Liujiagou and Sunjiagou formations

      图  11  锆石LA-ICP-MS U-Pb定年谐和图和频谱图

      Fig.  11.  Zircon LA-ICP-MS U-Pb concordia diagrams and histograms

      图  12  华北板块晚古生代-早中生代碎屑锆石及潜在源区U-Pb年龄(< 600 Ma)分布

      a.北京西山双泉组(Yang et al.,2006);b.燕山刘家沟组和孙家沟组(Ma et al.,2014);c,g.云冈-平鲁石盒子组上部;宁武-静乐刘家沟组(周瑞,2019);d.内蒙古隆起晚古生代花岗岩(Zhang et al.,2006);e.柳林地区刘家沟组和孙家沟组来自本次研究;f.延安地区石千峰组上部;济源地区石千峰组上部(Li et al.,2010彭深远等,2019);h.中亚造山带古生代至中生代地层碎屑锆石年龄(Li et al.,2011);i.沁水盆地石孙家沟组;k.洛阳-登封石千峰组上部和二马营组下部(Yang et al.,2017);l.北秦岭古生代花岗岩(Wang et al.,2009

      Fig.  12.  U-Pb ages (< 600 Ma) of potential sources detrital zircons from Late Paleozoic to Early Mesozoic in the North China craton

    • [1] Andersen, T., 2002. Correction of Common Lead in U-Pb Analyses That do not Report 204Pb. Chemical Geology, 192(1-2): 59-79. https://doi.org/10.1016/s0009-2541(02)00195-x
      [2] Boynton, W. V., 1984. Cosmochemistry of the Rare Earth Elements: Meteorite Studies. Rare Earth Element Geochemistry. Elsevier, Amsterdam, 63-114. https://doi.org/10.1016/b978-0-444-42148-7.50008-3
      [3] Cao, G. S., Fang, B. B., Sun, F. Y., et al., 2019. Maximum Sedimentary Age and Provenance of Pingdingshan Sandstone in the Southern Part of North China Block: Evidence from Detrital Zircon LA-ICP-MS U-Pb Age. Acta Petrologica Sinica, 35(8): 2518-2544(in Chinese with English abstract). doi: 10.18654/1000-0569/2019.08.13
      [4] Chen, L., Liang, C. Y., Liu, Y. J., et al., 2022. Geochronology and Provenance Analysis of the Xiufeng Formation in Mohe Basin: Implications for the Evolution of the Eastern Mongol-Okhotsk Ocean. Earth Science, 47(9): 3334-3353(in Chinese with English abstract).
      [5] Dickinson, W. R., Beard, L. S., Brakenridge, G. R., et al., 1983. Provenance of North American Phanerozoic Sandstones in Relation to Tectonic Setting. Geological Society of America Bulletin, 94(2): 222. https://doi.org/10.1130/0016-7606(1983)94222: ponaps>2.0.co;2 doi: 10.1130/0016-7606(1983)94222:ponaps>2.0.co;2
      [6] Dickinson, W. R., Gehrels, G. E., 2009. Use of U-Pb Ages of Detrital Zircons to Infer Maximum Depositional Ages of Strata: A Test against a Colorado Plateau Mesozoic Database. Earth and Planetary Science Letters, 288(1-2): 115-125. https://doi.org/10.1016/j.epsl.2009.09.013
      [7] Dong, Y. P., Santosh, M., 2016. Tectonic Architecture and Multiple Orogeny of the Qinling Orogenic Belt, Central China. Gondwana Research, 29(1): 1-40. https://doi.org/10.1016/j.gr.2015.06.009
      [8] Dong, Y. P., Sun, S. S., Santosh, M., et al., 2021. Central China Orogenic Belt and Amalgamation of East Asian Continents. Gondwana Research, 100: 131-194. https://doi.org/10.1016/j.gr.2021.03.006
      [9] Floyd, P. A., Leveridge, B. E., 1987. Tectonic Environment of the Devonian Gramscatho Basin, South Cornwall: Framework Mode and Geochemical Evidence from Turbiditic Sandstones. Journal of the Geological Society, 144(4): 531-542. https://doi.org/10.1144/gsjgs.144.4.0531
      [10] Fralick, P. W., Kronberg, B. I., 1997. Geochemical Discrimination of Clastic Sedimentary Rock Sources. Sedimentary Geology, 113(1/2): 111-124. https://doi.org/10.1016/s0037-0738(97)00049-3
      [11] Geng, Y. S., Wan, Y. S., Shen, Q. H., et al., 2000. Chronological Framework of the Early Precambrian Important Events in the Luliang Area, Shanxi Province. Acta Geologica Sinica, 74(3): 216-223(in Chinese with English abstract). doi: 10.3321/j.issn:0001-5717.2000.03.003
      [12] Han, G. Q., Liu, Y. J., Neubauer, F., et al., 2011. Origin of Terranes in the Eastern Central Asian Orogenic Belt, NE China: U-Pb Ages of Detrital Zircons from Ordovician-Devonian Sandstones, North Da Xing'an Mts. Tectonophysics, 511(3/4): 109-124. https://doi.org/10.1016/j.tecto.2011.09.002
      [13] Hao, Y. J., Shang, Q. Q., Ren, Y. S., et al., 2020. In Situ Analysis of Rare Earth Element Composition of Scheelite by LA-ICP-MS. Journal of Jilin University (Earth Science Edition), 50(4): 1029-1041(in Chinese with English abstract).
      [14] Ju, Y. W., Yu, K., Wang, G. Z., et al., 2021. Coupling Response of the Meso-Cenozoic Differential Evolution of the North China Craton to Lithospheric Structural Transformation. Earth-Science Reviews, 223: 103859. https://doi.org/10.1016/j.earscirev.2021.103859
      [15] Kong, L. y., Guo, P., Wan, J., et al., 2022. Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance. Earth Science, 47(4): 1333-1348(in Chinese with English abstract).
      [16] Li, D. P., Chen, Y. L., Wang, Z., et al., 2011. Detrital Zircon U-Pb Ages, Hf Isotopes and Tectonic Implications for Palaeozoic Sedimentary Rocks from the Xing-Meng Orogenic Belt, Middle-East Part of Inner Mongolia, China. Geological Journal, 46(1): 63-81. https://doi.org/10.1002/gj.1257
      [17] Li, H. Y., He, B., Xu, Y. G., et al., 2010. U-Pb and Hf Isotope Analyses of Detrital Zircons from Late Paleozoic Sediments: Insights into Interactions of the North China Craton with Surrounding Plates. Journal of Asian Earth Sciences, 39(5): 335-346. https://doi.org/10.1016/j.jseaes.2010.05.002
      [18] Li, S. Z., Jahn, B. M., Zhao, S. J., et al., 2017. Triassic Southeastward Subduction of North China Block to South China Block: Insights from New Geological, Geophysical and Geochemical Data. Earth-Science Reviews, 166: 270-285. https://doi.org/10.1016/j.earscirev.2017.01.009
      [19] Li, X. W., Liu, J., 2013. New Specimens of Pareiasaurs from the Upper Permian Sunjiagou Formation of Liulin, Shanxi and Their Implications for the Taxonomy of Chinese Pareiasaurs. Vertebrata Palasiatica, 51(3): 199-204(in Chinese).
      [20] Li, Z. Q., Li, F. J., Chen, Z. A., et al., 2022. Provenance of Late Mesozoic Strata and Tectonic Implications for the Southwestern Ordos Basin, North China: Evidence from Detrital Zircon U-Pb Geochronology and Hf Isotopes. Journal of Earth Science, 33(2): 373-394. https://doi.org/10.1007/s12583-021-1450-y
      [21] Liu, H. Y., 1991. Tectonic, Paleogeographic and Sedimentary Evolution of Late Precambrian in China. Chinese Journal of Geology, 26(4): 309-316(in Chinese with English abstract).
      [22] Liu, R. E., Huang, Y. M., Wei, X. F., et al., 2003. Analysis of Provenance of Late Paleozoic in the Northern Ordos Basin and Its Geological Significance. Journal of Mineralogy and Petrology, 23(3): 82-86(in Chinese with English abstract). doi: 10.3969/j.issn.1001-6872.2003.03.017
      [23] Liu, Y. J., Li, W. M., Ma, Y. F., et al., 2021. An Orocline in the Eastern Central Asian Orogenic Belt. Earth-Science Reviews, 221: 103808. https://doi.org/10.1016/j.earscirev.2021.103808
      [24] Ma, S. X., Meng, Q. R., Duan, L., et al., 2014. Reconstructing Late Paleozoic Exhumation History of the Inner Mongolia Highland along the Northern Edge of the North China Craton. Journal of Asian Earth Sciences, 87: 89-101. https://doi.org/10.1016/j.jseaes.2014.02.020
      [25] Mao, G. Z., Liu, C. Y., 2011. Application of Geochemistry in Provenance and Depositional Setting Analysis. Journal of Earth Sciences and Environment, 33(4): 337-348(in Chinese with English abstract).
      [26] McLennan, S. M., Hemming, S., McDaniel, D. K., et al., 1993. Geochemical Approaches to Sedimentation, Provenance, and Tectonics. In: Johnsson, M. J., Basu, A., eds., Processes Controlling the Composition of Clastic Sediments. Geological Society of America, 284: 21-40. https://doi.org/10.1130/spe284-p21
      [27] Meng, Q. R., Wu, G. L., Fan, L. G., et al., 2019. Tectonic Evolution of Early Mesozoic Sedimentary Basins in the North China Block. Earth-Science Reviews, 190: 416-438. https://doi.org/10.1016/j.earscirev.2018.12.003
      [28] Ouyang, S., Wang, R. N., 1985. Age Assignment of the Pingdingshan Member in Henan and Anhui Provinces. Petroleum Geology & Experiment, 7(2): 141-147, 167(in Chinese with English abstract).
      [29] Pei, F. P., Wang, Z. W., Cao, H. H., et al., 2014. Petrogenesis of the Early Paleozoic Tonalite in the Central Jilin Province: Evidence from Zircon U-Pb Chronology and Geochemistry. Acta Petrologica Sinica, 30(7): 2009-2019(in Chinese with English abstract).
      [30] Peng, S. Y., Yang, W. T., Wang, Y. P., et al., 2019. Detrital Zircon Chronology of the Lower-Middle Triassic Strata in Jiyuan Area and Its Implication for Provenance Analysis. Geological Science and Technology Information, 38(5): 126-137(in Chinese with English abstract).
      [31] Qin, Y., Liang, Y. H., Xing, J. L., et al., 2013. The Identification of Early Paleozoic O-Type Adakitic Rocks in Zhengxiangbaiqi Area, Inner Mongolia and Its Significance. Earth Science Frontiers, 20(5): 106-114(in Chinese with English abstract).
      [32] Rollinson, H., 1999. Petrology and Geochemistry of Metamorphosed Komatiites and Basalts from the Sula Mountains Greenstone Belt, Sierra Leone. Contributions to Mineralogy and Petrology, 134(1): 86-101. https://doi.org/10.1007/s004100050470
      [33] Roser, B. P., Korsch, R. J., 1988. Provenance Signatures of Sandstone-Mudstone Suites Determined Using Discriminant Function Analysis of Major-Element Data. Chemical Geology, 67(1-2): 119-139. https://doi.org/10.1016/0009-2541(88)90010-1
      [34] Shen, Q. H., Qian, X. L., 1995. Archean Rock Assemblages, Episodes and Tectonic Evolution of China. Acta Geoscientica Sinica, 16(2): 113-120(in Chinese with English abstract).
      [35] Sun, S. S., McDonough, W. F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. Geological Society, London, Special Publications, 42(1): 313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19
      [36] Taylor, S. R., McLennan, S. M., 1985. The Continental Crust: Its Composition and Evolution. Black well Scientific Publications, Oxford, 312.
      [37] Tucker, R. T., Roberts, E. M., Hu, Y., et al., 2013. Detrital Zircon Age Constraints for the Winton Formation, Queensland: Contextualizing Australia's Late Cretaceous Dinosaur Faunas. Gondwana Research, 24(2): 767-779. https://doi.org/10.1016/j.gr.2012.12.009
      [38] Wan, Y. S., Wilde, S. A., Liu, D. Y., et al., 2006. Further Evidence for ∼1.85 Ga Metamorphism in the Central Zone of the North China Craton: SHRIMP U-Pb Dating of Zircon from Metamorphic Rocks in the Lushan Area, Henan Province. Gondwana Research, 9(1/2): 189-197. https://doi.org/10.1016/j.gr.2005.06.010
      [39] Wang, F., Chen, F. K., Hou, Z. H., et al., 2009. Zircon Age Sand Sr-Nd-Hf Isotopic Paleozoic Granitoids in the Chongli-Chicheng Area, Northern Margin of the North China Block. Acta Petrologica Sinica, 25: 3057-3074 (in Chinese with English abstract).
      [40] Wang, J. Y., Yang, Y. C., Huang, Y. W., et al., 2016. Formation Ages and Tectonic Significance of Ophiolites in Wandashan Terrane of the Eastern Heilongjiang. Journal of Earth Sciences and Environment, 38(2): 182-195.
      [41] Wang, Y. C., Zhao, Y. Y., Liu, C. H., et al., 2020. Detrital Zircon Geochronology, Geochemistry and Geological Significance of Sandstone in the Ershierzhan Formation of the Mohe Basin. Acta Geologica Sinica, 94(3): 869-893(in Chinese with English abstract). doi: 10.3969/j.issn.0001-5717.2020.03.014
      [42] Wang, Y. P., 2019. Sedimentary and Provenance Characteristics of Middle Permian-Lower Triassic in Yiyang Area, Southern Margin of North China and Their Implications for Evolution of Basin-Mountain System (Dissertation). Henan Polytechnic University, Jiaozuo(in Chinese with English abstract).
      [43] Wei, Y. S., Feng, Z. Q., Yan, T., et al., 2021. Mesozoic Tectonic Evolution of the Central North China Craton: A Case Study from the Shanxi Province. Journal of Jilin University (Earth Science Edition), 1-25. (2021-08-26) (in Chinese with English abstract). https://kns.cnki.net/kcms/detail/22.1343.P.20210825.1417.001.html https://kns.cnki.net/kcms/detail/22.1343.P.20210825.1417.001.html
      [44] Wu, Q., Ramezani, J., Zhang, H., et al., 2021. High-Precision U-Pb Age Constraints on the Permian Floral Turnovers, Paleoclimate Change, and Tectonics of the North China Block. Geology, 49(6): 677-681. https://doi.org/10.1130/G48051.1
      [45] Xu, B., Zhao, P., Bao, Q. Z., et al., 2014. Preliminary Study on the Pre-Mesozoic Tectonic Unit Division of the Xing-Meng Orogenic Belt (XMOB). Acta Petrologica Sinica, 30(7): 1841-1857 (in Chinese with English abstract).
      [46] Yang, D. B., Yang, H. T., Shi, J. P., et al., 2017. Sedimentary Response to the Paleogeographic and Tectonic Evolution of the Southern North China Craton during the Late Paleozoic and Mesozoic. Gondwana Research, 49: 278-295. https://doi.org/10.1016/j.gr.2017.06.009
      [47] Yang, J. H., Wu, F. Y., Shao, J. A., et al., 2006. Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt, North China. Earth and Planetary Science Letters, 246(3/4): 336-352. https://doi.org/10.1016/j.epsl.2006.04.029
      [48] Yu, X. H., Wang, D. F., Zheng, J. M., 1994. Discussion on Relationship between Permian Sandstones Clastic Components and Its Tectonic Settings. Geoscience, 8(3): 299-307(in Chinese with English abstract).
      [49] Zhai, M., 2003. Palaeoproterozoic Tectonic History of the North China Craton: A Review. Precambrian Research, 122(1-4): 183-199. https://doi.org/10.1016/s0301-9268(02)00211-5
      [50] Zhai, M. G., Santosh, M., 2011. The Early Precambrian Odyssey of the North China Craton: A Synoptic Overview. Gondwana Research, 20(1): 6-25. https://doi.org/10.1016/j.gr.2011.02.005
      [51] Zhai, M. G., Peng, P., 2007. Paleoproterozoic Events in the North China Craton. Acta Petrologica Sinica, 23(11): 2665-2682(in Chinese with English abstract). doi: 10.3969/j.issn.1000-0569.2007.11.001
      [52] Zhang, J., Wang, Y. N., Zhang, B. H., et al., 2021. Tectonothermal Events in the Central North China Craton since the Mesozoic and Their Tectonic Implications: Constraints from Low-Temperature Thermochronology. Tectonophysics, 804(5): 228769. https://doi.org/10.1016/j.tecto.2021.228769
      [53] Zhang, J. Z., 2007. A Comparative Study on the Paleoproterozoic Strata in the Northern Section of the Luliang Mountain, Shanxi Province (Dissertation). China University of Geosciences, Beijing (in Chinese with English abstract).
      [54] Zhang, K., 1991. Tilloid at the Bottom of the Sedimentary Covers on the Margins of the Ordos Basin. Regional Geology of China, 10(1): 79-85(in Chinese with English abstract).
      [55] Zhang, S. H., Zhao, Y., Song, B., 2006. Hornblende Thermobarometry of the Carboniferous Granitoids from the Inner Mongolia Paleo-Uplift: Implications for the Tectonic Evolution of the Northern Margin of North China Block. Mineralogy and Petrology, 87(1): 123-141. https://doi.org/10.1007/s00710-005-0116-2
      [56] Zhang, S. H., Zhao, Y., Song, B., et al., 2007. Carboniferous Granitic Plutons from the Northern Margin of the North China Block: Implications for a Late Palaeozoic Active Continental Margin. Journal of the Geological Society, 164(2): 451-463. https://doi.org/10.1144/0016-76492005-190
      [57] Zhang, W., Jian, P., 2008. SHRIMP Dating of Early Paleozoic Granites from North Damaoqi, Inner Mongolia. Acta Geologica Sinica, 82(6): 778-787(in Chinese with English abstract). doi: 10.3321/j.issn:0001-5717.2008.06.007
      [58] Zhao, G. C., Cawood, P. A., 2012. Precambrian Geology of China. Precambrian Research, 222/223: 13-54. https://doi.org/10.1016/j.precamres.2012.09.017
      [59] Zhao, G. C., Cawood, P. A., Wilde, S. A., et al., 2000. Metamorphism of Basement Rocks in the Central Zone of the North China Craton: Implications for Paleoproterozoic Tectonic Evolution. Precambrian Research, 103(1-2): 55-88. https://doi.org/10.1016/S0301-9268(00)00076-0
      [60] Zhao, G. C., Sun, M., Wilde, S. A., et al., 2005. Late Archean to Paleoproterozoic Evolution of the North China Craton: Key Issues Revisited. Precambrian Research, 136(2): 177-202. https://doi.org/10.1016/j.precamres.2004.10.002
      [61] Zheng, W., Xu, X., Qi, Y. A., et al., 2021. Evolution of Terrestrial Triassic Ichnofossils and Ecological Significance in Western Henan Province. Earth Science, 1-23 (2021-07-21) (in Chinese with English abstract). https://kns.cnki.net/kcms/detail/42.1874.P.20210721.0834.002.html. https://kns.cnki.net/kcms/detail/42.1874.P.20210721.0834.002.html
      [62] Zhou, R., 2019. Study on the Relationship between Sedimentation and Tectonism of Late Paleozoic-Early Mesozoic Sediments in the North-Central North China Craton (Dissertation). Taiyuan University of Technology, Taiyuan (in Chinese with English abstract).
      [63] Zhou, R., Liu, D. N., Zhou, A. C., et al., 2019. A Synthesis of Late Paleozoic and Early Mesozoic Sedimentary Provenances and Constraints on the Tectonic Evolution of the Northern North China Craton. Journal of Asian Earth Sciences, 185: 104029. https://doi.org/10.1016/j.jseaes.2019.104029
      [64] Zhu, X. Q., Zhu, W. B., Ge, R. F., et al., 2014. Late Paleozoic Provenance Shift in the South-Central North China Craton: Implications for Tectonic Evolution and Crustal Growth. Gondwana Research, 25(1): 383-400. https://doi.org/10.1016/j.gr.2013.04.009
      [65] 曹高社, 方磅磅, 孙凤余, 等, 2019. 华北陆块南部平顶山砂岩的最大沉积年龄和物源区: 来自碎屑锆石LA-ICP-MS U-Pb年龄的证据. 岩石学报, 35(8): 2518-2544. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201908013.htm
      [66] 陈龙, 梁琛岳, 刘永江, 等, 2022. 漠河盆地绣峰组形成时代及物源分析: 对蒙古-鄂霍茨克洋东段演化的启示. 地球科学, 47(9): 3334-3353. doi: 10.3799/dqkx.2021.159
      [67] 耿元生, 万渝生, 沈其韩, 等, 2000. 吕梁地区早前寒武纪主要地质事件的年代框架. 地质学报, 74(3): 216–223. doi: 10.3321/j.issn:0001-5717.2000.03.003
      [68] 郝宇杰, 商青青, 任云生, 等, 2020. LA-ICP-MS原位分析白钨矿稀土元素. 吉林大学学报(地球科学版), 50(4): 1029-1041. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ202004009.htm
      [69] 孔令耀, 郭盼, 万俊, 等, 2022. 大别造山带中元古代变沉积岩碎屑锆石U-Pb年代学与Hf同位素特征及其地质意义. 地球科学, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096
      [70] 李兴文, 刘俊, 2013. 山西柳林孙家沟组锯齿龙类新材料及其分类学意义. 古脊椎动物学报, 51(3): 199-204. https://www.cnki.com.cn/Article/CJFDTOTAL-GJZD201303005.htm
      [71] 刘鸿允, 1991. 中国晚前寒武纪构造、古地理与沉积演化. 地质科学, 26(4): 309-316. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX199104001.htm
      [72] 刘锐娥, 黄月明, 卫孝锋, 等, 2003. 鄂尔多斯盆地北部晚古生代物源区分析及其地质意义. 矿物岩石, 23(3): 82-86. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200303016.htm
      [73] 毛光周, 刘池洋, 2011. 地球化学在物源及沉积背景分析中的应用. 地球科学与环境学报, 33(4): 337-348. https://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201104001.htm
      [74] 欧阳舒, 王仁农, 1985. 豫皖地区平顶山砂岩段地质时代的探讨. 石油实验地质, 7(2): 141-147, 167. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD198502008.htm
      [75] 裴福萍, 王志伟, 曹花花, 等, 2014. 吉林省中部地区早古生代英云闪长岩的成因: 锆石U-Pb年代学和地球化学证据. 岩石学报, 30(7): 2009-2019. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201407014.htm
      [76] 彭深远, 杨文涛, 王艳鹏, 等, 2019. 济源地区中-下三叠统碎屑锆石年代学特征及其物源分析. 地质科技情报, 38(5): 126-137. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201905013.htm
      [77] 秦亚, 梁一鸿, 邢济麟, 等, 2013. 内蒙古正镶白旗地区早古生代O型埃达克岩的厘定及其意义. 地学前缘, 20(5): 106-114. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201305008.htm
      [78] 沈其韩, 钱祥麟, 1995. 中国太古宙地质体组成、阶段划分和演化. 地球学报, 16(2): 113-120. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB502.000.htm
      [79] 王艳鹏, 2019. 华北南缘宜阳地区中二叠统-下三叠统沉积和物源特征及其对盆山系统演化的指示(博士学位论文). 焦作: 河南理工大学.
      [80] 王远超, 赵元艺, 刘春花, 等, 2020. 漠河盆地二十二站组砂岩年代学、地球化学及其地质意义. 地质学报, 94(3): 869-893. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE202003014.htm
      [81] 卫彦升, 冯志强, 闫涛, 等, 2021. 华北板块中部中生代构造演化: 以山西为例. 吉林大学学报(地球科学版), 1-25. (2021-08-26). https://kns.cnki.net/kcms/detail/22.1343.P.20210825.1417.001.html. https://kns.cnki.net/kcms/detail/22.1343.P.20210825.1417.001.html
      [82] 徐备, 赵盼, 鲍庆中, 等, 2014. 兴蒙造山带前中生代构造单元划分初探. 岩石学报, 30(7): 1841-1857. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201407001.htm
      [83] 于兴河, 王德发, 郑浚茂, 1994. 华北地区三叠系砂岩成分与构造背景关系的探讨. 现代地质, 8(3): 299-307. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ403.008.htm
      [84] 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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200711002.htm
      [85] 张建中, 2007. 山西吕梁山北段古元古代地层对比研究(硕士学位论文). 北京: 中国地质大学.
      [86] 张抗, 1991. 鄂尔多斯盆地边缘沉积盖层底部类冰碛岩的讨论. 中国区域地质, 10(1): 79-85. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD199101011.htm
      [87] 张维, 简平, 2008. 内蒙古达茂旗北部早古生代花岗岩类SHRIMP U-Pb年代学. 地质学报, 82(6): 778-787. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200806008.htm
      [88] 郑伟, 许欣, 齐永安, 等, 2021. 豫西地区陆相三叠纪遗迹化石演化及生态学意义. 地球科学, 1-23. (2021-07-21). https://kns.cnki.net/kcms/detail/42.1874.P.20210721.0834.002.html. https://kns.cnki.net/kcms/detail/42.1874.P.20210721.0834.002.html
      [89] 周瑞, 2019. 华北中北部晚古生代末期-早中生代沉积与构造作用的关系研究(博士学位论文). 太原: 太原理工大学.
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