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晚中生代东亚多板块汇聚与大陆构造体系的发展

张岳桥 董树文

张岳桥, 董树文, 2019. 晚中生代东亚多板块汇聚与大陆构造体系的发展. 地质力学学报, 25 (5): 613-641. DOI: 10.12090/j.issn.1006-6616.2019.25.05.059
引用本文: 张岳桥, 董树文, 2019. 晚中生代东亚多板块汇聚与大陆构造体系的发展. 地质力学学报, 25 (5): 613-641. DOI: 10.12090/j.issn.1006-6616.2019.25.05.059
ZHANG Yueqiao, DONG Shuwen, 2019. EAST ASIA MULTI-PLATE CONVERGENCE IN LATE MESOZOIC AND THE DEVELOPMENT OF CONTINENTAL TECTONIC SYSTEMS. Journal of Geomechanics, 25 (5): 613-641. DOI: 10.12090/j.issn.1006-6616.2019.25.05.059
Citation: ZHANG Yueqiao, DONG Shuwen, 2019. EAST ASIA MULTI-PLATE CONVERGENCE IN LATE MESOZOIC AND THE DEVELOPMENT OF CONTINENTAL TECTONIC SYSTEMS. Journal of Geomechanics, 25 (5): 613-641. DOI: 10.12090/j.issn.1006-6616.2019.25.05.059

晚中生代东亚多板块汇聚与大陆构造体系的发展

doi: 10.12090/j.issn.1006-6616.2019.25.05.059
基金项目: 

国家重点研发计划项目 2017YFC0601402

详细信息
    作者简介:

    张岳桥(1963-), 男, 教授, 博士生导师, 主要从事新构造、大地构造教学研究工作。E-mail:zhangyq@nju.edu.cn

  • 中图分类号: P54;P552

EAST ASIA MULTI-PLATE CONVERGENCE IN LATE MESOZOIC AND THE DEVELOPMENT OF CONTINENTAL TECTONIC SYSTEMS

  • 摘要: 东亚大陆原型形成于三叠纪印支造山运动旋回,其周邻环绕的三大洋(古太平洋、蒙古-鄂霍茨克洋、中特提斯洋)于早侏罗世初期几乎同时向东亚大陆俯冲,开启了东亚多板块汇聚历史。文章通过总结东亚大陆晚中生代构造变形和构造岩浆事件的新近研究成果,简述了东亚多板块汇聚产生的三个陆缘汇聚构造系统(北部蒙古-鄂霍次克碰撞造山带、东部与俯冲有关的增生造山系统、西南部班公湖-怒江缝合构造带)、陆内汇聚构造变形体系和大陆伸展构造体系。在此基础上,重新构建了东亚多板块汇聚大陆构造-岩浆演化的时间框架,将其划分为三个阶段:早侏罗世(200~170 Ma)周邻大洋板块初始俯冲阶段和陆缘裂解事件,中晚侏罗世-早白垩世早期(170~135 Ma)周邻陆缘碰撞造山或俯冲增生造山作用、陆内再生造山作用和汇聚构造体系的形成;中晚白垩世(135~80 Ma)大陆岩石圈的减薄作用和大陆伸展构造体系的发育。研究认为,晚中生代东亚多板块汇聚在时空上的有序演化和深浅构造的复合叠加,不仅产生了东亚大陆复杂的陆缘和陆内构造体系,同时控制了中国东部燕山期爆发式岩浆-成矿作用,也使东亚构造地貌发生东西翘变,早期陆缘汇聚产生的东部高原因晚期大陆岩石圈的减薄和伸展而垮塌。东亚大陆构造体系的形成和演化与联合古大陆的裂解同步,晚中生代东亚多板块汇聚完成了从东亚到欧亚大陆的演替,以东亚大陆为核心的多板块汇聚格局一直延续至新生代,可能成为未来超大陆形成的起点。

     

  • 图  1  东亚大陆晚中生代陆缘及陆内构造刚要图

    (左下角插图为东亚大陆周邻三个构造域分布简图)

    Figure  1.  Outline map showing Late Mesozoic marginal convergent belts and intracontinental deformation zones in East Asia

    (Inset at low left shows three tectonic realms and the location of East Asia)

    图  2  华南大陆晚中生代构造纲要图与陆缘早侏罗世岩浆弧和中晚侏罗世—早白垩世陆缘造山带根据文献[75, 101-103]编制)。

    Ⅰ—长乐—南澳断裂带; Ⅱ—晚侏罗世火山岩西界; Ⅲ—晚中生代火山岩西界; Ⅳ—晚中生代侵入岩西界

    Figure  2.  Outline map of Late Mesozoic tectonics in South China, delination of Early Jurassic marginal magmatic arc and Middle-Late Jurassic and Earth Cretaceous marginal orogeny (compiled from references [75, 101-103])

    (Ⅰ:Changle-Nanao Fault; Ⅱ:western boundary of late Jurassic volcanism; Ⅲ:western boundary of late Mesozoic vocanism; Ⅳ:western boundary of late Mesozoic intrusion)

    图  3  四川盆地东部侏罗山式褶皱带和武陵山箱状褶皱带深部结构特征和底部滑脱断层(根据文献[101]修改)

    Figure  3.  Interpreted seismic profile showing structural section of the Jura-type folds across east Sichuan and box-type folds across Wuling Shan and the main sole decollement (modified after reference [101])

    图  4  华北地块晚中生代逆冲褶皱变形系统构造纲要图

    Figure  4.  Outline map showing Late Mesozoic thrust-and-fold zones in North China

    图  5  秦岭构造带印支期碰撞造山作用与燕山期陆内造山作用构造模式

    Figure  5.  Tectonic evolutional model of Indosinian collisional and Yanshannian intracontinental oorgenesis across the Qinling belt

    图  6  郯庐断裂系及其中国北方晚中生代构造纲要图

    Figure  6.  The Tan-Lu fault system and late Mesozoic contractional structural map in northern China

    图  7  东亚大陆早侏罗世岩浆岩分布图

    Figure  7.  Early Jurassic magmatic rock distribution in East Asia

    图  8  郯庐左旋走滑断裂系及其与蒙古—鄂霍次克碰撞造山带和秦岭—大别陆内造山带之间的运动学联系

    Figure  8.  The Tan-Lu sinistral strike-slip fault system in East Asia and its kinematic link between the Mongolia-Okhst collisional orogen and the Qinling-Dabie intracontinental orogen

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  • 收稿日期:  2019-08-20
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