古老造山带洋板块地层<sup>*</sup>

doi:10.7605/gdlxb.2022.01.003

古地理学报 ›› 2022, Vol. 24 ›› Issue (1): 33-44. doi: 10.7605/gdlxb.2022.01.003

古老造山带洋板块地层^*

崔慧琪^1,2, 许淑梅^1,2,3, 李三忠^1,2,3, 舒鹏程^1,2, 马慧磊^1,2, 孔家豪^1,2

1 中国海洋大学海底科学与探测技术教育部重点实验室,山东青岛 266100;
2 中国海洋大学海洋地球科学学院,山东青岛 266100;
3 海洋高等研究院/深海圈层与地球系统前沿中心,山东青岛 266100

收稿日期:2021-08-05 修回日期:2021-09-23 出版日期:2022-01-01 发布日期:2022-01-24
通讯作者: 许淑梅,女,1970年生,博士,教授,长期从事沉积学和盆地分析的教学和研究工作。E-mail: xsm@ouc.edu.cn。
作者简介:崔慧琪,女,1998年生,硕士研究生,专业方向为盆地分析和层序地层学。E-mail: 2360284331@qq.com。
基金资助:
*国家自然科学基金项目(编号: 91958109,91958214,42121005)、中央高校基本科研业务专项(编号: 202172003)、国家自然科学基金委员会—山东海洋科学中心联合项目(编号: U1606401)和山东省泰山学者攀登计划项目(编号: tspd20210315)联合资助

Reconstruction of Ocean Plate Stratigraphy from the ancient orogen

Cui Hui-Qi^1,2, Xu Shu-Mei^1,2,3, Li San-Zhong^1,2,3, Shu Peng-Cheng^1,2, Ma Hui-Lei^1,2, Kong Jia-Hao^1,2

1 Key Lab of Submarine Geosciences and Prospecting Techniques,Ministry of Education, Ocean University of China, Shandong Qingdao 266100,China;
2 College of Marine Geosciences,Ocean University of China,Shandong Qingdao 266100,China;
3 Institute of Advanced Oceanography/Frontiers Science Center for Deep Ocean Multispheres and Earth System, Shandong Qingdao 266100,China

Received:2021-08-05 Revised:2021-09-23 Online:2022-01-01 Published:2022-01-24
Contact: Xu Shu-Mei,born in 1970, professor, is engaged in studies on sedimentology and basin analysis. E-mail: xsm@ouc.edu.cn.
About author:Cui Hui-Qi,born in 1998,is a candidate for Master Degree. Her research interests are basin analysis and sequence stratigraphy. E-mail: 2360284331@qq.com.
Supported by:
Co-funded by the Shandong Provincial Natural Science Foundation,China(No. ZR2019MD037)and the National Natural Science Foundation of China(No.41776059)

摘要/Abstract

摘要：

重点分析和总结了由前寒武纪增生复合体和造山带混杂岩重建的古老造山带洋板块地层,包括由英国威尔士安格尔西岛新元古代莫纳超群混杂岩重建的太平洋洋板块地层、由澳大利亚西北部皮尔巴拉早太古代克里夫维尔绿岩带重建的古印度洋洋板块地层。澳大利亚东皮尔巴拉地块大理石坝地区早太古代玄武岩—硅质岩—碎屑岩序列与日本二叠纪—三叠纪洋板块地层在岩石组成和地球化学特征方面具有高度的相似性,这一认识将为早太古代洋板块地层的沉积环境从高热流洋脊扩张区经过热点向低热流海沟陆源碎屑沉积区转变这一过程提供有力支持。从增生造山带洋板块地层保存的岩石记录看,不同年代洋板块地层的主要物质组成和岩石类型相似,因此在地球38亿年的演化进程中,洋壳扩张、海洋沉积、俯冲及增生的过程并没有显著变化;但随着时间推移,年轻造山带洋板块性质和洋板块地层组成与古老造山带相比,可能会发生一些变化。就古老造山带洋板块地层而言,前寒武纪的地幔温度略高,太古代局部熔融显著,熔融量大大超过洋壳扩张速率,因而没有形成席状岩墙群。

关键词: 前寒武纪, 古老造山带, 增生复合体, 混杂岩, 洋板块地层

Abstract:

The paper focuses on reconstruction of the Oceanic Plate Stratigraphy (OPS)from the Precambrian accretionary complexes and mélange of ancient orogenic belts,including the Pacific OPS reconstructed from the Neoproterozoic Mona Supergroup mélange in Anglesey,Wales,United Kingdom,and the Paleo-Indian OPS reconstructed from the Early Archean Cleaverville greenstone belt,Pilbara,northwest Australia. The early Archean basalt-silicate-clastic sequence in the Marble Bar area of the East Pilbara Block of Australia is highly similar to the Permian-Triassic ocean plate strata of Japan in rock composition and geochemical characteristics. This conclusion will provide strong support for evolution of the sedimentary environments of the early Archean OPS from the high-heat flow ridge spreading area,through the hot spot,to the low-heat flow trench,terrigenous clastic depositional zone. According to the rock records of the OPS in the accretive orogenic belt,the main composition and rock types of the OPS strata from the Archean to the present are similar. Therefore,the processes of ocean spreading,deposition,subduction and accretion have not changed significantly during the Earth's 3.8-byr-history. However,the oceanic plate properties and the oceanic plate stratigraphic composition of young orogenic belts may have changed with time. Precambrian mantle temperature was slightly high,and the degree of partial melting was high in the Archean. The melting amount greatly exceeded the expansion rate of the ocean crust,so the sheet dike group did not form in ancient oceanic crust.

Key words: Precambrian, ancient orogenic belt, accretionary complex, m&#x000e9, lange, Oceanic Plate Stratigraphy

中图分类号:

P547

崔慧琪, 许淑梅, 李三忠, 舒鹏程, 马慧磊, 孔家豪. 古老造山带洋板块地层^*[J]. 古地理学报, 2022, 24(1): 33-44.

Cui Hui-Qi, Xu Shu-Mei, Li San-Zhong, Shu Peng-Cheng, Ma Hui-Lei, Kong Jia-Hao. Reconstruction of Ocean Plate Stratigraphy from the ancient orogen[J]. JOPC, 2022, 24(1): 33-44.

http://www.gdlxb.cn/CN/Y2022/V24/I1/33

参考文献

[1]Agard P,Yamato P,Jolivet L,Burov E.2009. Exhumation of ocean blueschists and eclogites in subduction zones: timing and mechanisms. Earth-Science Reviews, 92: 53-79.
[2]Asanuma H,Okada Y,Fujisaki W,Suzuki K,Sato T,Sawaki Y,Sakata S,Yamamoto S,Hirata T,Maruyama S,Windley B F.2015. Reconstruction of ocean plate stratigraphy in the Gwna Group,NW Wales: implications for the subduction and accretion process of a latest Pro terozoic trench forearc. Tectonophysics, 662: 195-207.
[3]Barley M E.1993. Volcanic,sedimentary and tectonostratigraphic environments of the 3.46 Ga Warrawoon a mega-sequence: a review. Precambrian Research, 60: 47-67.
[4]Blewett R S.2002. Archaean tectonic processes: a case for horizontal shortening in the North Pilbara Granite-Greenstone Terrane,Western Australia. Precambrian Research, 113: 87-120.
[5]Bolhar R,Von Kranendonk M J,Kamber B S.2005. A trace element study of siderite-jasper banded iron formation in the 3.45 Ga Warrawoona Group,Pilbara Craton: formation from hydrothermal fluids and shallow seawater. Precambrian Research, 137: 93-114.
[6]Bradley D C.2011. Secular trends in the geologic record and the supercontinent cycle. Earth-Science Reviews, 108: 16-33.
[7]Compston W,Wright A E,Toghill P.2002. Dating the Late Precambrian volcanicity of England and Wales. Journal of the Geological Society, 159(3): 323-339.
[8]Condon D,Prave A R.2000. Two from Donegal: Neoproterozoic glacial episodes on the northeast margin of Laurentia. Geology, 28: 951-954.
[9]Dallmeyer R D,Gibbons W.1987. The age of blueschist metamorphism on Anglesey,North Wales: evidence from ⁴⁰Ar/³⁹Ar mineral dates of the Penmynydd schists. Journal of Geological Society of London, 144: 843-850.
[10]Eriksson A,Hiatt E E,Laflamme M,Lenehard N,Long D G F,Miall A D,Mints M V,Pufahi P K,Sarkar S,Simpson E L, Williams G E.2012. Secular changes in sedimentation systems and sequence stratigraphy. Gondwana Research, 24: 468-489.
[11]Gibbons W,Hor$\acute{a}$k J M. 1996. The evolution of the Neoproterozoic Avalonian subduction system: evidence from the British Isles. In: Nance R D,Thompson M D(eds). A valonian and Related Peri-Gondwana Terranes of the Circum-North Atlantic. Geological Society of America Special Paper, 304: 269-280.
[12]Green M G,Sylvester P J,Buick R.2000. Growth and recycling of early Archaean continental crust: geochemical evidence from the Coonteru nah and Warrawoona Groups,Pilbara Craton,Australia. Tectonophysics, 322(1-2): 69-88.
[13]Greenly E.1919. The geology of Anglesey. Memoir,Geological Survey of Great Britain,2. London:HMSO,1-980.
[14]Kato Y,Ohta I,Tsunematsu T,Watanabe Y,Isozaki Y,Maruyama S,Imai N.1998. Rare earth element variations in mid-Archean banded iron formations: implications for the chemistry of ocean and continent and platetectonics. Geochimica et Cosmochimica Acta, 62: 3475-3497.
[15]Kato Y,Nakao K,Isozaki Y.2002. Geochemistry of Late Permian to Early Triassic pelagic cherts from southwest Japan: implications for an oceanic redox change. Chemical Geology, 182(1): 15-34.
[16]Kato Y,Nakamura K.2003. Origin and global tectonic significance of Early Archean cherts from the Marble Bar greenstone belt,Pilbara Craton,Western Australia. Precambrian Research, 125(3-4): 191-243.
[17]Kawai T,Windley B F,Terabayashi M,Yamamoto H,Maruyama S,Isozaki Y.2006. Mineral isograds and metamorphic zones of the Anglesey blueschist belt,UK: implications for the metamorphic development of a Neoproterozoic subduction-accretion complex. Journal of Metamorphic Geology, 24: 591-602.
[18]Kawai T,Windley B F,Terabayashi M,Yamamoto H,Maruyama S,Omori S,Shibuya T,Sawaki Y,Isozaki Y.2007. Geotectonic framework of the Blueschist Unit on Anglesey-Lleyn,UK,and its role in the deve lopment of a Neoproterozoic accretionary orogen. Precambrian Research, 153: 11-28.
[19]Kimura K,Hori R.1993. Offscraping accretion of Jurassic chert-clastic complexes in the Mino-Tamba Belt,central Japan. Journal of Structural Geology, 15(2): 145-161.
[20]Kimura G,Maruyama S,Isozaki Y,Terabayashi M.1996. Well-preserved underplating structure of the jadeitized Franciscan complex,Pacheco Pass,California. Geology, 24(1): 75-78.
[21]Kitajima K,Maruyama S,Utsunomiya S,Liou J G.2001. Seafloor hydrothermal alteration at an Archaean mid-ocean ridge. Journal of Metamorphic Geology, 19(5): 583-599.
[22]Krapez B,Eisenlohr B.1998. Tectonic setting of Archaean(3325-2775^Ma)crustal-supracrustal belts in the West Pilbara Block. Precambrian Research, 88: 173-205.
[23]Kusky T M,Windley B F,Safonova I,Wakita K,Wakabayashi J,Polat A,Santosh M.2013. Recognition of ocean plate stratigraphy in accretionary orogens through Earth history: a record of 3.8 billion years of sea floor spreading,subduction,and accretion. Gondwana Research, 24: 501-547.
[24]Maruyama S,Kawai T,Windley B F.2010. Ocean plate stratigraphy and its imbrication in an accretionary orogen: the Mona Complex,Anglesey-Lleyn,Wales,UK. In: Kusky T M,Zhai M G,Xiao W(eds). The Evolving Continents: Understanding Processes of Continental Growth. Geological Society,London,Special Publications, 338: 55-75.
[25]Matsuda T,Isozaki Y.1991. Well-documented travel history of Mesozoic pelagic chert in Japan: from remote ocean to subduction zone. Tectonics, 10: 475-499.
[26]Ohta H,Maruyama S,Takashi E,Watanabe Y,Kato Y.1996. Field occurrence,geochemistry and petrogenesis of the Archean Mid-Oceanic Ridge Basalts(AMORBs)of the Cleaverville area,Pilbara Craton,Western Australia. Lithos, 37(2-3): 199-221.
[27]Osozawa S.1994. Plate reconstruction based upon age data of Japanese accretionary complexes. Geology, 22: 1135-1138.
[28]Robinson P,Malpas J,Dilek Y.2008. The significance of sheeted dike complexes in ophiolites. GSA Today, 18: 4-10.
[29]Strachan R A,Taylor G K(eds). 1990. Avalonian and Cadomian Geology of the North Atlantic. Blackie,Glasgow:1-252.
[30]Terabayashi M,Masafa Y,Ozawa H.2003. Archean ocean-floor metamorphism in the North Pole area,Pilbara Craton,Western Australia. Precambrian Research, 127: 167-180.
[31]Trindada R I F,Macouin M.2007. Palaeolatitude of glacial deposits and palaeogeography of Neoproterozoic ages. Comptes Rendus Geoscience, 339: 200-211.
[32]Tucker R D,Pharaoh T C.1991. U-Pb zircon ages for Late Precambrian igneous rocks in southern Britain. Journal of Geological Society of London, 148: 435-443.
[33]Wagoner Kranendonk M J,Smithies R H,Hickman A H,Champion D C. 2007. Paleoarchean development of a continental nucleus: the East Pilbara terrane of the Pilbara Craton,western Australia. In: Wagoner Kranendonk M J,Smithies R H,Bennett V C(eds).Earth’s Oldest Rocks. Amsterdam: Elsevier,307-337.
[34]Wood M.2012. The historical development of the term‘mélange’ and its relevance to the Precambrian geology of Anglesey and the Lleyn Peninsula in Wales, UK. Journal of Geography, 121: 168-180.
[35]Young G M.2012. Secular changes at the Earth’s surface: evidence from palaeosols,some sedimentary rocks,and paleoclimatic perturbations of the Proterozoic Eon. Gondwana Research, 24: 453-467.

选择文件类型/文献管理软件名称

选择包含的内容

古老造山带洋板块地层^*

Reconstruction of Ocean Plate Stratigraphy from the ancient orogen

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 5

编辑推荐

Metrics

本文评价

[1]	旷红伟, 彭楠, 王玉冲, 白华青, 祁柯宁, 柳永清. 臼齿碳酸盐岩: 解密前寒武纪海洋化学性质的钥匙^*[J]. 古地理学报, 2023, 25(1): 1-22.
[2]	马慧磊, 许淑梅, 李三忠, 舒鹏程, 崔慧琪, 孔家豪. 年轻造山带洋板块地层^*[J]. 古地理学报, 2022, 24(1): 11-32.
[3]	许淑梅, 孔家豪, 李三忠, 舒鹏程, 马慧磊, 崔慧琪. 洋板块地层学的概念、模式、组成及失序变化^*[J]. 古地理学报, 2022, 24(1): 1-10.
[4]	张连昌, 兰彩云, 王长乐, 彭自栋, 佟小雪, 李文君, 董志国. 古元古代大氧化事件(GOE)前后海洋环境的变化: 来自华北条带状铁建造(BIF)岩相学和地球化学的证据^*[J]. 古地理学报, 2020, 22(5): 827-840.
[5]	梅冥相. 冥古宙的地层学属性:了解地球形成初期古地理背景和演变历史的重要线索^*[J]. 古地理学报, 2016, 18(4): 513-524.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

古老造山带洋板块地层*

Reconstruction of Ocean Plate Stratigraphy from the ancient orogen

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 5

编辑推荐

Metrics

本文评价

古老造山带洋板块地层^*