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    欧亚北极区东部区域地质与构造演化

    李学杰 姚永坚 杨楚鹏 李波 李涛

    李学杰, 姚永坚, 杨楚鹏, 李波, 李涛, 2017. 欧亚北极区东部区域地质与构造演化. 地球科学, 42(3): 315-324. doi: 10.3799/dqkx.2017.024
    引用本文: 李学杰, 姚永坚, 杨楚鹏, 李波, 李涛, 2017. 欧亚北极区东部区域地质与构造演化. 地球科学, 42(3): 315-324. doi: 10.3799/dqkx.2017.024
    Li Xuejie, Yao Yongjian, Yang Chupeng, Li Bo, Li Tao, 2017. Regional Geological Features and Tectonic Evolution in the Eastern Euroasian Arctic. Earth Science, 42(3): 315-324. doi: 10.3799/dqkx.2017.024
    Citation: Li Xuejie, Yao Yongjian, Yang Chupeng, Li Bo, Li Tao, 2017. Regional Geological Features and Tectonic Evolution in the Eastern Euroasian Arctic. Earth Science, 42(3): 315-324. doi: 10.3799/dqkx.2017.024

    欧亚北极区东部区域地质与构造演化

    doi: 10.3799/dqkx.2017.024
    基金项目: 

    国土资源部专项项目 GZH201200601

    详细信息
      作者简介:

      李学杰 (1964-),男,教授级高工,主要从事海洋地质与区域地质的调查与研究工作.ORCID:0000-0002-8606-3752.E-mail: xuejieli@yeah.net

    • 中图分类号: P56

    Regional Geological Features and Tectonic Evolution in the Eastern Euroasian Arctic

    • 摘要: 欧亚北极东部地区资源丰富,但由于区域地质构造复杂,勘探程度低,盆地分布及其发育的构造背景仍存在很大的争议.在大量收集整理区域地质文献的基础上编制了该区构造简图,并对区域地质构造及其演化进行梳理.该区主要构造单元包括:上扬斯克-科雷马造山带、北极阿拉斯加-楚科塔微板块、科雷马-奥莫隆复合超地体、南阿纽伊缝合带等.早侏罗世至早白垩世,随着美亚海盆的张开,北极阿拉斯加-楚科塔微板块裂离加拿大北部陆缘,并随着Anui-Anvil洋的关闭,与科雷马-奥莫隆超地体及亚洲大陆北缘碰撞,形成新西伯利亚-楚科奇造山带-布鲁克斯造山带及南阿纽伊缝合带.上扬斯克-科雷马造山带是晚侏罗世-早白垩世科雷马-奥莫隆超地体与西伯利亚克拉通边缘的碰撞结果.

       

    • 图  1  欧亚北极东部地区位置

      Fig.  1.  Location of the eastern Euroasian Arctic region

      图  2  欧亚北极东部构造简图

      Fig.  2.  Tectonic scheme of the eastern Euroasian Arctic region

      图  3  上扬斯克-科雷马造山带及邻区构造简图

      Fig.  3.  Tectonic scheme of the Verkhoyansk-Kolyma orogen

      图  4  始新世时美亚海盆与北极阿拉斯加-楚科塔微板块环境

      L.利亚霍夫群岛,A.安茹群岛,D.德朗群岛,据Pease (2011)修改

      Fig.  4.  The Canada basin and Arctic Alaska-Chukotka microplate in Eocene

      图  5  大利亚霍夫岛过南阿纽伊缝合线西端N-S向剖面示意

      引自Kuzmichev (2009)

      Fig.  5.  Schematic N-S profile through the western end of the South Anyui suture in big Lyakhov island

      图  6  美亚海盆构造演化模式

      Grantz et al.(2011)修改

      Fig.  6.  Model of tectonic evolution of Amerasia basin

      图  7  上扬斯克-科雷马造山带演化模型

      Oxman (2003)修改

      Fig.  7.  Model of geodynamic evolution of the Verkhoyansk-Kolyma orogen

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    • 收稿日期:  2016-09-30
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