Composition and Evolution of the Ancient Basement of the North China Craton
WAN Yu-sheng1, DONG Chun-yan1, XIE Hang-qiang1, ZHENG Jian-ping2, LIU Shou-jie1,MA Ming-zhu1, XIE Shi-wen1, REN Peng1, SUN Hui-yi1, LIU Dun-yi1
1. Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China; 2. State Key Laboratory of Geological Processes and Mineral Resources, Faculty of Earth Sciences, China University of Geosciences, Wuhan, Hubei 430074, China
Abstract：We carried out integrated geological, geochronological and geochemical studies on typical early Precambrian areas of the North China Craton, such as Anshan-Benxi, eastern Hebei, western Shandong and Yinshan, and synthesized the general geological records of the Archean basement relating to Archean crust formation and evolution of the North China Craton. This study also revealed that the Ordos basement was involved in a widespread late Paleoproterozoic tectono-thermal event. We defined and outlined three ancient terranes containing abundant 3.8~2.6 Ga rocks for the first time in the North China Craton, namely the Eastern Ancient Terrane, Southern Ancient Terrane and Central Ancient Terrane.
万渝生，董春艳，颉颃强，郑建平，刘守偈，马铭株，谢士稳，任鹏，孙会一，刘敦一. 华北克拉通古老大陆地壳组成及演化[J]. 中国地质调查, 2015, 2(3): 1-4.
WAN Yu-sheng, DONG Chun-yan, XIE Hang-qiang, ZHENG Jian-ping, LIU Shou-jie,MA Ming-zhu, XIE Shi-wen, REN Peng, SUN Hui-yi, LIU Dun-yi. Composition and Evolution of the Ancient Basement of the North China Craton. , 2015, 2(3): 1-4.
[1] 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: 2785-2792. [2] 董春艳, 万渝生, 张玉海, 等. 鞍山地区东山杂岩3.3 ~ 3.1 Ga岩浆作用:地球化学和锆石定年[J]. 岩石学报, 2013, 29: 414-420. [3] 马铭株, 万渝生, 徐仲元, 等. 华北克拉通大青山地区古元古代晚期钾长伟晶岩脉:锆石SHRIMP定年和Hf同位素组成[J]. 地质通报, 2012, 31: 825-833. [4] 马铭株, 徐仲元, 张连昌, 等. 内蒙古武川县西乌兰不浪地区早前寒武纪变质基底锆石SHRIMP定年及Hf同位素组成[J]. 岩石学报, 2013, 29: 501-516. [5] 万渝生,刘敦一,王世进, 等. 华北克拉通鲁西地区早前寒武纪表壳岩重新划分和BIF形成时代[J]. 岩石学报, 2012, 28:3457-3475. [6] 万渝生,董春艳,颉颃强, 等. 华北克拉通早前寒武纪条带状铁建造形成时代: SHRIMP 锆石U-Pb定年[J].地质学报, 2012, 86: 1447-1478. [7] Dong C Y, Wan Y S, Xu Z Y, et al. Late Paleoproterozoic kondalites in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating[J]. Science China Earth Sciences, 2013, 56: 115-125. [8] Dong C Y, Wan Y S, Wilde S A, et al. Early Paleoproterozoic supracrustal rocks at Daqingshan in the Khondalite Belt of North China Craton: Evidence from SHRIMP zircon U-Pb dating[J]. Gondwana Research, 2014, 25: 1535-1553. [9] Liu S J, Dong C Y, Xu Z Y, et al. Paleoproterozoic episodic magmatism and high-grade metamorphism in the North China Craton: Evidence from SHRIMP zircon dating of magmatic suites from the Daqingshan area[J]. Geological Journal, 2013, 48: 429-455. [10] Liu S J, Wan Y S, Sun H Y, et al. Paleo-to Eoarchean crustal materials in eastern Hebei, North China Craton: New evidence from SHRIMP U-Pb dating and in-situ Hf isotopic studies in detrital zircons of supracrustal rocks[J]. Journal of Asian Earth Sciences, 2014, 78: 4-17. [11] Ma M Z, Wan Y S, Santosh M, et al. Decoding multiple tectonothermal events in zircons from single rock samples: SHRIMP zircon U-Pb data from the late Neoarchean rocks of Daqingshan, North China Craton[J]. Gondwana Research, 2012,22: 810-827. [12] Ma Q, Zheng J P, Griffin W L, et al. Triassic “adakitic” rocks in an extensional setting (North China): Melts from the cratonic lower crust[J]. Lithos, 2012, 149: 159-173. [13] Wan Y S, Wang S J, Liu D Y, et al.Redefinition of depositional ages of Neoarchean supracrustal rocks in western Shandong Province, China: SHRIMP U-Pb zircon dating[J]. Gondwana Research, 2012, 21:768-784. [14] Wan Y S, Dong C Y, Liu Y D, et al. Zircon ages and geochemistry of late Neoarchean syenogranites in the North China Craton: A review[J]. Precambrian Research, 2012, 222/223: 265-289. [15] Wan Y S, Liu D Y, Nutman A, et al. Multiple 3.8-3.1 Ga tectono-magmatic events in a newly discovered area of ancient rocks (the Shengousi Complex), Anshan, North China Craton[J]. Journal of Asian Earth Sciences, 2012, 54/55:18-30. [16] Wan Y S, Xu Z Y, Dong C Y, et al. Episodic Paleoproterozoic (~2.45, ~1.95 and ~1.85 Ga) mafic magmatism and associated high temperature metamorphism in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating and whole-rock geochemistry[J]. Precambrian Research, 2013, 224:71-93. [17] Wan Y S, Zhang Y H, Williams I S, et al. Extreme zircon O isotopic compositions from 3.8 to 2.5 Ga magmatic rocks from the Anshan area, North China Craton[J]. Chemical Geology, 2013, 352: 108-124. [18] 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. [19] Wan Y S, Dong C Y, Wang S J, et al. Middle Neoarchean magmatism in western Shandong, North China Craton: SHRIMP zircon dating and LA-ICP-MS Hf isotope analysis[J]. Precambrian Research,2014, 255:865-884. [20] Zheng J P, Griffin W L, Ma Q, et al. Accretion and reworking beneath the North China Craton[J]. Lithos, 2012, 149: 61-78.
2015, Vol. 2 
