吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 335-348.doi: 10.13278/j.cnki.jjuese.201502101
• 地质与资源 • 下一篇
李学杰1, 姚永坚1, 杨楚鹏1, 陈振林2, 汪俊1, 张亚玲1
Li Xuejie1, Yao Yongjian1, Yang Chupeng1, Chen Zhenlin2, Wang Jun1, Zhang Yaling1
摘要:
北极地区范围很广,北极圈面积达2 100×104 km2,区域地质复杂。通过对北极地区区域地质编图,笔者认为前寒武纪主要由波罗的、劳伦和西伯利亚三大克拉通,以及其间的微板块或地块组成。主要造山带包括新元古代-早寒武世的贝加尔造山带、晚志留世-早石炭世的加里东造山带、晚古生代-早中生代的海西造山带、晚中生代的上扬斯克造山带、新西伯利亚造山带与楚科奇-布鲁克斯造山带。根据北极地区区域地质构造特征,显生宙以来经历的构造事件大致包括:新元古代-早寒武世的贝加尔运动,致使波罗的古陆与斯瓦尔巴-喀拉地块碰撞造山;晚泥盆世-早石炭世的加里东运动,在劳伦古陆周边形成规模巨大的加里东造山带;晚古生代的海西运动,波罗的古陆与西伯利亚古陆的碰撞造山形成海西造山带;北极阿拉斯加-楚科奇微板块裂离加拿大边缘,侏罗纪加拿大海盆开始张开;早白垩世,阿拉斯加-楚科奇微板块继续与西伯利亚碰撞,阿纽伊洋(Anyui Ocean)消亡,形成上扬斯克-布鲁克斯造山带。受北极调查程度影响,许多问题有待进一步研究。
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| [1] Filatova N I, Khain V E. The Arctida Craton and Neoproterozoic-Mesozoic Orogenic Belts of the Circum-Polar Region[J]. Geotectonics, 2010, 44(3): 203-227.[2] 李学杰, 万玲, 万荣胜, 等. 北冰洋地质构造及其演化[J]. 极地研究, 2010, 22(3): 271-285. Li Xuejie, Wan Ling, Wan Rongsheng, et al. The Structure and Tectonic Revolution of Arctic Ocean[J]. Chinese Journal of Polar Research, 2010, 22(3): 271-285.[3] Drachev S S, Malyshev N A, Nikishin A M. Tectonic History and Petroleum Geology of the Russian Arctic Shelves: An Overview[C]//Vinnig, B A, Pickering S C. Petroleum Geology: From Mature Basins to New Frontiers-Proceedings of the 7th Petroleum Geology Conference. London: London Geological Society, 2010:591-619. Doi: 10.1144/0070591.[4] 李学杰, 万荣胜, 万玲, 等. 北冰洋的地形地貌与地质构造特征[C]//南海地质研究:2009.北京:地质出版社, 2010:56-68. Li Xuejie, Wan Rongsheng, Wan Ling, et al. The Topography and Tectonics of the Arctic Ocean[C]//Geological Research of South China Sea:2009. Beijing:Geological Publishing House, 2010:56-68.[5] 李学杰, 姚永坚, 韩冰, 等. 北极地区区域地质及美亚海盆的演化[J]. 吉林大学学报:地球科学版, 2012, 42(增刊2):224-233. Li Xuejie, Yao Yongjian, Han Bing, et al. Regional Geology of the Arctic Polar Area and the Evolution of the Amerasian Basin[J]. Journal of Jilin University: Earth Science Edition, 2012, 42(Sup.2): 224-233.[6] Khain V E, Polyakova I D, Filatova N I. Tectonics and Petroleum Potential of the East Arctic Province[J]. Russian Geology and Geophysics, 2009, 50: 334-345.[7] Li Z X, Bogdanova S V, Collins A S, et al. Assembly, Configuration, and Break-Up History of Rodinia: A Synthesis[J]. Precambrian Research, 2008, 160: 179-210.[8] Shipilov E V, Vernikovsky V A. The Svalbrd-Kala Plates Junction: Structure and Geodynamic History[J]. Russian Geology and Geophysics, 2010, 51: 58-71.[9] Spencer A M, Embry A F, Gautier D L, et al. An Overview of the Petroleum Geology of the Arctic[C]//Spencer A M, Embry A F, Gautier D L, et al. Arctic Petroleum Geology. London: London Geological Society, Memoirs, 2011, 35:1-15.[10] Pease V, Scott R A. Crustal Affinities in the Arctic Uralides, Northern Russia: Significance of Detrital Zircon Ages from Neoproterozoic and Paleozoic Sediments in Novaya Zemlya and Taimyr[J]. Journal of the Geological Society, 2009, 166: 517-527.[11] Pease V. Eurasian Orogensand Arctic Tectonics: An Overview[C]//Spencer A M, Embry A F, Gautier D L, et al. Arctic Petroleum Geology. London: London Geological Society, Memoirs, 2011, 35:311-324.[12] Kuzmichev A B. Where Does the South Anyui Suture Go in the New Siberian Islandsand Laptev Sea?: Implications for the Amerasia Basin Origin[J]. Tectonophysics, 2009, 463: 86-108.[13] Pavlov V E, Gallet Y, Petrov P Yu, et al. Uy Series and Late Riphean Sills of the Uchur-Maya Area: Isotopic and Palaeomagnetic Data and the Problem of the Rodinia Supercontinent[J]. Geotectonics, 2002, 36: 278-292.[14] Lawver L A, GrantzA, Gahagan L M. Plate Kinematic Evolution of the Present Arctic Region Since the Ordovician[C]//Miller E L, Grantz A, Klemperer S L. Tectonic Evolution of the Bering Shelf-Chukchi Sea-Arctic Margin and Adjacent Landmasses. Boulder:Geol Soc America, 2002: 333-358.[15] Pushcharovsky Yu M. Tectonics of the Arctic Ocean[J].Geotektonika, 1976, 6(2): 3-14.[16] Golonka J, Bocharova N Y, Ford D, et al. Paleogeographic Reconstruction and Basins Development of the Arctic[J]. Marine and Petroleum, 2003, 20: 211-248.[17] Puchkov V N.Tectonics of the Urals: Moden Concepts[J].Geotectonics, 1997, 31(4): 294-312.[18] Vernikovsky V A, Vernikovskaya A E, Chernykh A I, et al. Petrology and Geochemistry of the Riphean Ophiolites in North Taimyr[J]. Geol Geofiz, 1996, 37(1): 113-129.[19] Golonka J, Bocharova N Y, Ford D, et al. Paleogeographic Reconstruction and Basins Development of the Arctic[J]. Marine and Petroleum, 2003, 20: 211-248.[20] Gee D G, Tebenkov A M. Svalbard: A Fragmentof Laurentian Margin[J]. Geological Society, Memoirs, 2004, 30: 191-206.[21] Metelkin D V, Vernikovsky V A, Kazansky A Yu, et al. Paleozoic History of the Kara Microcontinent and Its Relation to Siberia and Baltica: Paleomagnetism, Paleogeography and Tectonics[J].Tectonophysics, 2005, 398: 225-243.[22] Lorenz H, Männik P, Gee D, et al. Geology of the Severnaya Zemlya Archipelagoand the North Kara Terrane in the Russian High Arctic[J]. Int J Earth Sci:Geol Rundsch, 2008, 97:519-547.[23] Kos'ko M K, Cecile M P, Harrison J C, et al.Geology of Wrangel Island Between Chukchi and East Siberian Seas[J].Russia Geol Surv Canada Bull, 1993, 461: 1-101.[24] Kos'ko M K.Terranes of the Russian East Arctic Shelf[J].Dokl Earth Sci, 2007, 413(2): 183-186.[25] Pease V, Dovzhicova, Beliakova L, et al. Late Neoproterozoic Granitoid Magmatismin the Basement to the Pechora Basin, NW Russia: Geochemical Constraints Indicate Westward Subduction Beneath NE Baltica[J]. Geological Society, Memoirs, 2004, 30: 75-85.[26] Baluev A S. Geodynamics of the Riphean Stage of Evolution of the Northern Passive Margin of the EastEuropean Craton[J].Geotectonics, 2006, 40 (3): 183-196.[27] Roberts D, Olovyanishnikov V. Structural and Tectonic Development of the Timanide Orogen[C]//The Neoproterozoic Timanide Orogen of Eastern Baltica. London: London Geological Society, Memoirs, 2004, 30: 47-57.[28] Ritzmann O, Faleide J I.Caledonian Basement of the Western Barents Sea[J]. Tectonophysics, 2007, 26: 1-20.[29] Breivik A J, Mjelde R, Grogan P, et al. Caledonide Development Offshore-Onshore Svalbard Based on Ocean Bottom Seismometer, Conventional Seismic and Potential Field Data[J]. Tectonophysics, 2005, 401: 79-117.[30] Klemperer S L, Miller E L, Scholl D W.Crustal Structure of the Bering and Chukchi Shelves: Deep Seismic Refnection Profiles Across the North American Continent Between Alaska and Russia[C]//Miller E L, Grantz A, Klemperer S L. Tectonic Evolution of the Bering Shelf-Chukchi Sea-Arctic Margin and Adjacent Landmasses. Boulder: Geol Soc America, 2002: 1-24.[31] KoragoEu A, Kovaleva G N, Lopatin B G, et al. The Precambrian Rocks of Novaya Zemlya[C]//The Neoproterozoic Timanide Orogen of Eastern Baltica. London: London Geological Society, Memoirs, 2004, 30: 135-143.[32] Pogrebitskiy Yu E, Novaya Zemlya, Vaigach Island. Geological Structure and Miragenia[C]//Niiga-Vniio Keangeologiya. St Petersburg:, 2004:205.[33] Vinokurov I Yu, Belyaev V I, Egorov A S, et al. Deep-Crustal Model and Evolution of Barents-Kara Region[C]//Geology of Polar Regions of the Earth. Moscow:Materials of Xlii Tectonic Conference, I Geos, 2009: 102-106.[34] Uflyand A K, Natapov L M, Lopatin V M, et al. To the Taimyr Tectonic Nature[J]. Geotectoniks, 1991, 6: 76-93.[35] Vernikovsky V. Riphean and Paleozoic Metamorphic Complexes of the Taimyr Foldbelt: Condition of Formation[J]. Petrol, 1995, 3: 55-72.[36] Männik P, Bogolepova O G, Pöldvere A, et al. New Data on Ordovician-Silurian Conodontsand Stratigraphy from the Severnay Zemlya Archipelago, Russian Arctic[J]. Geological Magazine, 2009, 146(4):497-516.[37] Drachev S S, Johnson G L, Laxon S, et al. Main Structural Elements of the Eastern Russian Arctic Continental Margin Derived from Satellite Gravity and Multichannel Seismic Reflection Data[C]//Kassens H, Bauch H A. Land-Ocean Systems in the Siberian Arctic: Dynamics and History. Berlin: Springer, 1999: 667-682.[38] Drachev S S, Elistratov A V, Savostin L A. Structure and Seismostratigraphy of the East Siberian Sea Shelf Along the Indigirka Bay-Jeannette Island Seismic Profile[J]. Doklady Earth Sciences, 2001, 377: 293-297.[39] Grantz A, Hart P, Childers V A. Geology and Tectonic Development of the Amerasia and Canada Basins, Arctic Ocean[C]//Spencer A M, Embry A F, Gautier D L, et al.Arctic Petroleum Geology. London: London Geological Society, Memoirs, 2011, 35: 771-799.[40] Sokolov S D, Bondarenko G Ye, Morozov O L, et al. South Anui Suture, Northeast Arctic Russia[C]//Miller E L, Grantz A, Klemperer S L. Tectonic Evolution of the Bering Shelf-Chukchi Sea-Arctic Margin and Adjacent Landmasses.[S.l.]: Geol Soc America, Boulder, 2002: 209-223.[41] Houseknecht D, Bird K. Geology and Petroleum Potential of the Rifted Margins of Arctic Alaska and the Chukchi Borderland[C]//AAPG International Conference and Exhibition. Calgary:[s.n.], 2010:12-15. |
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