Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (4): 1042-1055.doi: 10.13278/j.cnki.jjuese.201604105

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Combined NE China Blocks: Tectonic Evolution and Supercontinent Reconstructions

Zhou Jianbo, Shi Aiguo, Jing Yan   

  1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2016-02-29 Online:2016-07-26 Published:2016-07-26
  • Supported by:

    Supported by the Natural Science Foundation of China (41390441, 41190075, 41272241) and National Innovation Experiment Project for University Students(2016-06-07).

Abstract:

NE China has traditionally been considered as the eastern part of the Central Asian Orogenic Belt (CAOB), located between the Siberia and North China cratons. They constitute Paleozoic accretionary margins to the Siberia and the North China cratons, terminated to the east by the Paleo-Pacific orogens. In detail, NE China is the key area for understanding the geodynamics between the CAOB and Paleo-Pacific subduction. The tectonic units of the combined NE China blocks (NEC) include the Jiamusi-Khanka blocks in the northeast, the Xing'an and Songliao blocks in the central area, and the Erguna block in the northwest. The basement rocks in NEC constitute a common khondalitic sequence of Neoproterozoic with high grade metamorphism occurred at ~500 Ma. The Paleozoic sediments also show slimier sequences in most blocks in the NE China, suggesting that the combined NE China blocks (NEC) might be have similar or same tectonic evolutions during that time. The boundary between these blocks show following new evidences: 1)the suture zone between the Eerguna and Xing'an blocks is the Early Paleozoic Toudaoqiao-Xinlin suture and not the Mesozoic Derbugan fault. 2)the emplacement time of the Hegenshan-Heihe suture between the Xing'an and Songlao blocks is the Late Carboniferous and not the Mesozoic as recently reported. 3)the Paleo-Asian Ocean between the combined NE China blocks (NEC) and North China block is along the Xar Moron-Changchun suture and the collision timing is the Triassic. 4)the collision timing of the Jilin-Heilongjiang high pressure metamorphic belt (Ji-Hei HP belt) between the Jiamusi-Khanka and Songliao blocks is the switch time when end of the CAOB and beginning the Paleo-Pacific subduction at sometime between 210 and 180 Ma, and 5)the Nadanhada accretionary complex is the only records for the Paleo-Pacific subuduction from Late Triassic to Early Cretaceous in NE China. In addition, we also focus on the evidences of the both typical tectono-magmatic events and Paleontologic signatures, and reconstruction of the NEC from Gondwana to Pangea supercontinent.

Key words: combined NE China blocks (NEC), Pan-African basement, Paleozoic cover, location and timing of the suture zone, supercontinent reconstruction of the from Gondwana to Pangea

CLC Number: 

  • P541

[1] ?engör A M C, Natal'in B A, Burtman V S. Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia[J]. Nature,1993, 364: 299-307.

[2] 任纪舜,王作勋,陈炳蔚,等.从全球看中国大地构造:中国及临区大地构造图简要说明[M].北京:地质出版社,1999: 4-32. Ren Jishun, Wang Zuoxun, Chen Bingwei, et al. The Tectonics of China from a Global View:A Guide to the Tectonic Map of China and Adjacent Regions[M]. Beijing:Geological Publishing House, 1999: 4-32. [HQ]

[3] 唐克东,王莹,何国琦,等.中国东北及邻区大陆边缘构造[J].地质学报, 1995,69(2):16-30. Tang Kedong, Wang Ying, He Guoqi, et al.Continental-Margin Structure of Northeast China and Its Adjacent Areas[J]. Acta Geologica Sinica,1995, 69(2): 16-30.

[4] Li J Y. Permian Geodynamic Setting of Northeast China and Adjacent Regions: Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26: 207-224.

[5] Zhou J B, Wilde S A. The Crustal Accretion History and Tectonic Evolution of the NE China Segment of the Central Asian Orogenic Belt[J]. Gondwana Research, 2013, 223 (4):1365-1377.

[6] Zhou J B, Cao J L, Wilde S A, et al. Paleo-Pacific Subduction-Accretion: Evidence from Geochemical and U-Pb Zircon Dating of the Nadanhada Accretionary Complex, NE China[J].Tectonics, 2014, 33:2014TC003637.

[7] 李锦轶, 牛宝贵, 宋彪, 等.长白山北段地壳的形成与演化[M].北京: 地质出版社, 1999:32-50. Li Jinyi, Niu Baogui, Song Biao, et al. Crustal Formation and Evolution of Northern Changbai Mountains, Northeast China[M]. Beijing:Geological Publishing House, 1999:32-50.

[8] Wilde S A, Zhang X Z, Wu F Y. Extension of A Newly-Identified 500 Ma Metamorphic Terrain in Northeast China: Further U-Pb SHRIMP Dating of the Mashan Complex, Heilongjiang Province, China[J]. Tectonophysics,2000, 328: 115-130.

[9] Wilde S A, Wu F Y, Zhang X Z. Late Pan-African Magmatism in Northeastern China: SHRIMP U-Pb Zircon Evidence for Igneous Ages from the Mashan Complex[J]. Precambrian Research, 2003, 122:311-327.

[10] 曹熹, 党增欣, 张兴洲,等.佳木斯复合地体[M].长春:吉林科技出版社,1992:1-126. Cao Xi, Dang Zengxin, Zhang Xingzhou, et al. The Composite Jiamusi Terrane[M]. Changchun:Jilin Science & Technology Publishing House, 1992:1-126.

[11] 姜继圣.麻山群孔兹岩系主期区域变质作用及演化[J].岩石矿物学杂志, 1992, 11(2):97-108. Jiang Jisheng. Peak Regional Metamorphism of the Khondalite Series of Mashan Group and Its Evolution[J]. Acta Petrologica et Mineralogica, 1992, 11(2):97-108.

[12] 黑龙江省地质矿产局.黑龙江省区域地质志[M].北京:地质出版社,1993:1-734. Heilongjiang Bureau of Geology and Mineral Resources. Regional Geology of Heilongjiang Province[M].Beijing: Geological Publishing House, 1993: 1-734.

[13] 邵济安.中朝板块北缘中段地壳演化[M].北京:北京大学出版社, 1991:1-136. Shao Ji'an. Crustal Evolution in the Middle Part of the Northern Margin of Sino-Korean Plate[M]. Beijing: Peking University Press,1991:1-136.

[14] Jia D C, Hu R Z, Lu Y, et al. Collision Belt Between the Khanka Block and the North China Block in the Yanbian Region, Northeast China[J]. Journal of Asian Earth Sciences,2004, 23: 211-219.

[15] Shi G R, Zhan L P. A Mixed Mid-Permian Marine Fauna from the Yanji Area, Northeastern China: A Paleobiogeographical Reinterpretation[J]. The Island Arc, 1996, 5:385-395.

[16] Shi G R.Marine Permian in East and NE Asia: An Overview of Biostratigraphy, Palaeobiogeography and Palaeogeographical Implications[J]. Journal of Asian Earth Sciences, 2006, 26 (3/4): 175-206.

[17] Zhou J B, Wilde S A, Zhao G C, et al. Was the Easternmost Segment of the Central Asian Orogenic Belt Derived from Gondwana or Siberia: An Intriguing Dilemma? [J] Journal of Geodynamics, 2010, 50:300-317.

[18] Zhou J B, Wilde S A, Zhao G C, et al. Pan-African Metamorphic and Magmatic Rocks of the Khanka Massif, NE China: Further Evidence Regarding Their Affinity[J]. Geological Magazine,2010, 147(5):737-749.

[19] 孙跃武,郎嘉彬,葛文春,等. 松辽盆地外围晚古生代地层研究[R]. 长春:吉林大学,2012. Sun Yuewu, Lang Jiabing, Ge Wenchun, et al. Research on the Late Paleozoic Strata Around the Songliao Basin[R]. Changchun: Jilin University, 2012.

[20] 董策. 佳木斯地块构造演化:来自晚古生代沉积-火山岩的制约[D].长春:吉林大学,2009:1-121. Dong Ce.Tectonic Evolution of the Jiamusi Massif: Constrains from Late Paleozoic Sedimentary-Volcanic Rocks[D]. Changchun:Jilin University,2009:1-121.

[21] 王颖, 张福勤, 张大伟, 等. 松辽盆地南部变闪长岩SHRIMP锆石U-Pb年龄及其地质意义[J]. 科学通报,2006, 51(15):1877-1883. Wang Ying, Zhang Fuqin, Zhang Dawei, et al. Zircon SHRIMP U-Pb Dating of Meta-Diorite from the Basement of the Songliao Basin and Its Geological Significance[J]. Chinese Science Bulletin, 2006, 51(15):1877-1883.

[22] 裴福萍,许文良,杨德彬, 等.松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义[J].科学通报, 2007,52(24):942-948. Pei Fuping, Xu Wenliang, Yang Debin, et al. Zircon U-Pb Geochronology of Basement Metamorphic Rocks in the Songliao Basin[J]. Chinese Science Bulletin, 2007, 52(24):942-948.

[23] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41:1-30.

[24] Zhou J B, Wilde S A, Zhang X Z, et al. Detrital Zircons from Phanerozoic Rocks of the Songliao Block. NE China: Evidence and Tectonic Implications[J]. Journal of Asian Earth Sciences, 2012, 47:21-34.

[25] 权京玉, 迟效国, 张蕊, 等.松嫩地块东部新元古代东风山群碎屑锆石LA-ICP-MS U-Pb年龄及其地质意义[J].地质通报,2013,32(2/3):353-364. Quan Jingyu, Chi Xiaoguo, Zhang Rui, et al. LA-ICP-MS U-Pb Geochronology of Detrital Zircon from the Neoproterozoic Dongfengshan Group in Songnen Masiff and Its Geological Significance[J]. Geological Bulletin of China, 2013,32(2/3):353-364.

[26] 高福红,王枫,许文良, 等.小兴安岭"古元古代"东风山群的形成时代及其构造意义:锆石U-Pb年代学证据[J].吉林大学学报(地球科学版),2013,43(2):440-456. Gao Fuhong, Wang Feng, Xu Wenliang, et al. Age of the "Paleoproterozoic" Dongfengshan Group in the Lesser Xing'an Range, NE China, and Its Tectonic Implications: Constraints from Zircon U-Pb Geochronology[J].Journal of Jilin University(Earth Science Edition), 2013, 43(2):440-456.

[27] Rong J Y, Boucot A J, Su Y Z. Biogeographical Analysis of Late Silurian Brachiopod Faunas, Chiefly from Asia and Australia[J]. Lethaia, 1995,28: 39-60.

[28] Wu G, Chen Y C, Chen Y J, et al. Zircon U-Pb Ages of the Metamorphic Supracrustal Rocks of the Xinghuadukou Group and Granitic Complexes in the Argun Massif of the Northern Great Hinggan Range, NE China, and Their Tectonic Implications[J]. Journal of Asian Earth Sciences, 2012, 49:214-233.

[29] 周建波, 张兴洲, Wilde S A, 等. 中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J].岩石学报, 2011,27(4):1235-1245. Zhou Jianbo, Zhang Xingzhou, Wilde S A, et al. Confirming of the Heilongjiang ~500 Ma Pan-African Khondalite Belt and Its Tectonic Implications[J]. Acta Petrologica Sinica, 2011,27(4):1235-1245.

[30] Zhou J B, Wilde S A, Zhang X Z, et al. A >1 300 km Late Pan-African Metamorphic Belt in NE China: New Evidence from the Xing'an Block and Its Tectonic Implications[J]. Tectonophysics,2011, 509: 280-292.

[31] Zhou J B, Wilde S A, Zhang X Z, et al. Pan-African Metamorphic Rocks of the Erguna Block in the Great Xing'an Range, NE tgChina: Evidence for the Timing of Magmatic and Metamorphic Events and Their Tectonic Implications[J]. Tectonophysics, 2011, 499(1/2/3/4):105-117.

[32] Rong J Y, Cocks L R M. Global Diversity and Endemism in Early Silurian (Aeronian) Brachiopods[J]. Lethaia, 2014,47: 77-106.

[33] Kojima S. Mesozoic Terrane Accretion in Northeast China, Sikhote-Alin and Japan Regions[J].Palaeogeography, Palaeoclimatology, Palaeoecology,1989,69:213-232.

[34] 周建波,韩杰, Wilde S A,等.吉林[CD1]黑龙江高压变质带的初步厘定:证据和意义[J].岩石学报,2013,29(2):386-398. Zhou J B, Han J, Wilde S A,et al.A Primary Study of the Jilin-Heilongjiang High-Pressure Metamorphic Belt: Evidence and Tectonic Implacations[J].Acta Petrologica Sinica, 2013,29(2):386-398.

[35] Wu F Y, Yang J H, Lo C H,et al. Jiamusi Massif in China: A Jurassic Accretionary Terrane in the Western Pacific[J]. The Island Arc, 1990, 16: 156-172.

[36] Zhou J B, Wilde S A, Zhang X Z, et al. The Onset of Pacific Margin Accretion in NE China: Evidence from the Heilongjiang High-Pressure Metamorphic Belt[J]. Tectonophysics, 1999,478: 230-246.

[37] Zhou J B, Wilde S A, Zhao G C, et al. New SHRIMP U-Pb Zircon Ages from the Heilongjiang Complex in NE China: Constraints on the Mesozoic Evolution of NE China[J]. American Journal of Science, 2010, 310: 1024-1053.

[38] 曹从周,杨芳林,田昌裂. 内蒙古贺根山地区蛇绿岩和中朝板块和西伯利亚板块之间的缝合带位置[C]//唐克东.中国北方板块构造论文集:第1集.北京: 地质出版社, 1986: 64-86. Cao Congzhou, Yang Fanglin, Tian Changlie. The Ophiolite in Hegenshan District, Nei Mongol and the Position of Suture Line Between Sino-Korean and Siberian Plates[C]//Tang Kedong. Contributions to the Project of Plate Tectonics in Northern China:No.1. Beijing:Geological Publishing House, 1986: 64-86.

[39] Zhou J B, Han J, Zhao G C.The Emplacement Time of the Hegenshan Ophiolite: Constraints from the Unconformably Overlying Paleozoic Strata[J].Tectonophysics,2015(662): 398-415.

[40] 郑常青,周建波,金巍,等.大兴安岭地区德尔布干断裂带北段构造年代学研究[J].岩石学报,2009,25(8):1989-2000. Zheng Changqing, Zhou Jianbo, Jin Wei, et al. Geochronology in the North Segment of the Derbugan Fault Zone, Great Xing'an Range, NW China[J].Acta Petrologica Sinica, 25(8): 1989-2000.

[41] 李瑞山. 新林蛇绿岩[J]. 黑龙江地质,1991,2(1):19-31. Li Ruishan. Xinlin Opholite[J]. Heilongjiang Geology, 1991,2(1):19-31.

[42] 佘宏全,李进文,向安平,等.大兴安岭中北段原岩锆石 U-Pb 测年及其与区域构造演化关系[J]. 岩石学报,2012,28(2): 571-594. She Hongquan,Li Jinwen,Xiang Anping,et al.U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution[J]. Acta Petrologica Sinica,2012, 28(2):571-594.

[43] 冯志强. 大兴安岭北段古生代构造-岩浆演化[D].长春:吉林大学,2015. Feng Zhiqiang.The Palezoic Tectono-Magmatic Evolution of the Northern Great Xing'an Range[D]. Changchun:Jilin University,2015.

[44] Zhou J B, Wang B, Wilde S A, et al. Geochemistry and U-Pb Zircon Dating of the Toudaoqiao Blueschists in the Great Xing'an Range, Northeast China, and Tectonic Implications[J]. Journal of Asian Earth Sciences, 2015, 97:197-210.

[45] Han J, Zhou J B,Wang B, et al. The Final Collision of the CAOB: Constraint from the Zircon U-Pb Dating of the Linxi Formation, Inner Mongolia[J].Geoscience Frontiers ,2015,6(2):211-225.

[46] Cocks L R M,Torsvik T H. Siberia, the Wandering Northern Terrane, and Its Changing Geography Through the Palaeozoic[J].Earth-Science Reviews, 2007, 82: 29-74.

[47] 王成文, 孙跃武, 李宁, 等. 东北地区晚古生代地层分布规律[J].地层学杂志,2009, 33(1):56-61. Wang Chengwen, Sun Yuewu, Li Ning, et al. On the Distribution of the Late Palaeozoic Strate in Northeast China[J]. Journal of Stratigraphy, 2009, 33(1):56-61.

[48] Veevers J J.Gondwanaland from 650-500 Ma Assembly Through 320 Ma Merger in Pangea to 185-100 Ma Breakup: Supercontinental Tectonics Via Stratigraphy and Radiometric Dating [J].Earth-Science Reviews, 2004,28 :1-132.

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