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    三江昌宁-孟连带原-古特提斯构造演化

    王保弟 王立全 王冬兵 尹福光 贺娟 彭智敏 闫国川

    王保弟, 王立全, 王冬兵, 尹福光, 贺娟, 彭智敏, 闫国川, 2018. 三江昌宁-孟连带原-古特提斯构造演化. 地球科学, 43(8): 2527-2550. doi: 10.3799/dqkx.2018.160
    引用本文: 王保弟, 王立全, 王冬兵, 尹福光, 贺娟, 彭智敏, 闫国川, 2018. 三江昌宁-孟连带原-古特提斯构造演化. 地球科学, 43(8): 2527-2550. doi: 10.3799/dqkx.2018.160
    Wang Baodi, Wang Liquan, Wang Dongbing, Yin Fuguang, He Juan, Peng Zhimin, Yan Guochuan, 2018. Tectonic Evolution of the Changning-Menglian Proto-Paleo Tethys Ocean in the Sanjiang Area, Southwestern China. Earth Science, 43(8): 2527-2550. doi: 10.3799/dqkx.2018.160
    Citation: Wang Baodi, Wang Liquan, Wang Dongbing, Yin Fuguang, He Juan, Peng Zhimin, Yan Guochuan, 2018. Tectonic Evolution of the Changning-Menglian Proto-Paleo Tethys Ocean in the Sanjiang Area, Southwestern China. Earth Science, 43(8): 2527-2550. doi: 10.3799/dqkx.2018.160

    三江昌宁-孟连带原-古特提斯构造演化

    doi: 10.3799/dqkx.2018.160
    基金项目: 

    中国地质调查局项目 DD20160016

    国家自然科学基金项目 41773026

    国家重点研发计划项目 2015CB452601

    国家自然科学基金项目 41603038

    详细信息
      作者简介:

      王保弟(1975-), 男, 研究员, 博士, 从事青藏高原地质研究工作

    • 中图分类号: P54

    Tectonic Evolution of the Changning-Menglian Proto-Paleo Tethys Ocean in the Sanjiang Area, Southwestern China

    • 摘要: 昌宁-孟连特提斯洋的构造演化及其原特提斯与古特提斯的转换方式一直是青藏高原及邻区基础地质研究中最热门的科学问题之一.根据新的地质调查资料、研究成果并结合分析数据,系统总结了三江造山系不同构造单元地质特征,讨论了昌宁-孟连特提斯洋早古生代-晚古生代的构造演化历史.通过对不同构造单元时空结构的剖析和对相关岩浆、沉积及变质作用记录的分析,认为昌宁-孟连结合带内共存原特提斯与古特提斯洋壳残余,临沧-勐海一带发育一条早古生代岩浆弧带,前人所划基底岩系"澜沧岩群"应为昌宁-孟连特提斯洋东向俯冲消减形成的早古生代构造增生杂岩,滇西地区榴辉岩带很可能代表了俯冲增生杂岩带发生了深俯冲,由于弧-陆碰撞而迅速折返就位,这一系列新资料及新认识表明昌宁-孟连结合带所代表的特提斯洋在早古生代至晚古生代很可能是一个连续演化的大洋.在此基础上,结合区域地质资料,构建了三江造山系特提斯洋演化的时空格架及演化历史,认为其经历了早古生代原特提斯大洋扩张、早古生代中晚期-晚古生代特提斯俯冲消减与岛弧带形成、晚二叠世末-早三叠世主碰撞汇聚、晚三叠世晚碰撞造山与盆山转换等阶段.

       

    • 图  1  青藏高原构造格架简图(a)及西南三江地区大地构造单元划分(b)

      Wang et al.(2014a)修改.KL.阿尼玛卿-昆仑结合带;GL.甘孜-理塘结合带;JS.金沙江结合带;AL.哀牢山结合带;NL.北澜沧江结合带;SL.南澜沧江结合带;LS.龙木错-双湖结合带;CM.昌宁-孟连结合带;BN.班公湖-怒江结合带;YL.印度-雅鲁藏布江结合带

      Fig.  1.  Tectonic framework of the Tibetan Plateau (a) and tectonic unit division of the Sanjiang Orogen and surrounding areas (b)

      图  2  三江南段昌宁-孟连弧盆系构造单元及前侏罗纪岩浆作用时空分布

      数据引用同表 1

      Fig.  2.  Simplified geological map of the Changning-Menglian orogenic system, showing the temporal-spatial distribution of pre-Jurassic magmatic rocks

      图  3  昌宁-孟连结合带铜厂街(a)、南汀河(b)、牛井山(c)和曼信(d)蛇绿混杂岩地质简图

      图a据陈莉等(2015);图b据云南省地质调查院(2017,中华人民共和国1:5万香竹林、勐勇、勐撒、懂过、耿马县、安雅、勐库7幅区域地质调查报告);图c据王冬兵等(2016);图d据云南省地质矿产局(1984,中华人民共和国1:20万孟连幅区域地质调查报告)

      Fig.  3.  Simple geological maps of the Tongchangjie (a), Nantinghe (b), Niujingshan (c) and Manxin (d) ophiolites in the Changning-Menglian suture zone

      图  4  昌宁-孟连结合带蛇绿混杂岩基性岩构造环境图解

      南汀河数据来自Wang et al.(2013a);铜厂街数据来自陈莉等(2015);干龙塘数据来自赖绍聪等(2010)

      Fig.  4.  Tectonic environments diagram of mafic rocks in the Changning-Menglian ophiolite mélange

      图  5  昌宁-孟连蛇绿混杂岩基性岩REE配分及微量元素蛛网图

      数据来源同图 4

      Fig.  5.  Chondrite-normalized REE pattern and primitive mantle normalized trace element spider diagram of mafic rocks in the Changning-Menglian ophiolite mélange

      图  6  三江南段早古生代岩浆岩构造环境判别图解

      大中河数据来自毛晓长等(2012);惠民数据来自Nie et al.(2015);大平掌数据来自Hehmann et al.(2013);双江数据来自云南省地质调查院,2017.中华人民共和国1:5万香竹林、勐勇、勐撒、懂过、耿马县、安雅、勐库7幅区域地质调查报告

      Fig.  6.  Tectonic environments diagram of Early Paleozoic magmatic rocks in the southern part of Sanjiang River

      图  7  昌宁-孟连蛇绿混杂岩基性岩REE配分模式(a)和微量元素蛛网图(b)

      数据来源同图 6

      Fig.  7.  The chondrite-normalized REE pattern (a) and PM-normalized trace element spider diagram (b) of Early Paleozoic magmatic rocks of the Changning-Menglian area

      图  8  西南三江昌宁-孟连弧盆系演化模式简图

      潘桂棠等(2012)修改

      Fig.  8.  Schematic illustrations of the characteristics and evolution of the Changning-Menglian Orogenic System in the Sanjiang River

      表  1  三江南段早古生代蛇绿混杂岩及岩浆岩年龄信息统计

      Table  1.   Statistical of age information of Early Paleozoic ophiolite and magmatic rocks in the southern part of Sanjiang River

      构造单元 地点 样品编号 岩石名称 测试方法 年龄(Ma) 误差(Ma) 来源
      昌宁-孟连结合带 南汀河 11NTH-4 辉长岩 LA-ICPMS 439.0 2.4 Wang et al.(2013a, 2013b)
      11NTH-6 堆晶辉长岩 LA-ICPMS 443.6 4.0
      12NTH-1 堆晶辉长岩 LA-ICPMS 439.0 5.8 Wang et al.(2013b)
      12NTH-5 堆晶辉长岩 LA-ICPMS 453.9 5.6
      双江勐库 PM029-17-1 堆晶斜长岩 LA-ICPMS 470.8 5.3 刘桂春等(2017)
      牛井山 D0017-1 英云闪长岩 LA-ICPMS 468.0 2.0 王冬兵等(2016)
      老南掌 D0010-1-2 玄武岩 LA-ICPMS 449.0 8.4 孙载波等(2017)
      早古生代岩浆岩 惠民 D008 玄武岩 LA-ICPMS 456.0 3.0 Nie et al.(2015)
      D009 安山岩 LA-ICPMS 456.0 7.0
      D010 英安岩 LA-ICPMS 459.0 14.0
      大平掌 辉钼矿 WR Re-Os 442.4 5.6 李文昌等(2010)
      辉钼矿 WR Re-Os 428.8 6.1
      DP-103 花岗闪长斑岩 LA-ICPMS 401.0 1.7 汝珊珊等(2012)
      Y-1 英安岩 LA-ICPMS 428.9 1.5 Lehmann et al.(2013)
      大中河 DZH01-1 凝灰岩 LA-ICPMS 418.0 5.1 毛晓长等(2012)
      大中河 DZH01-1 凝灰岩 LA-ICPMS 421.0
      双江 GMTK-1 绿片岩 LA-ICPMS 451.7 2.1 云南省地质调查院(2017)
      双江 XSBD-1-1 绿片岩 LA-ICPMS 453.5 0.9
      粟义 11ML-57H 变火山岩 LA-ICPMS 462.0 6.0 Xing et al.(2017)
      下载: 导出CSV
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