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东北亚活动大陆边缘中生代构造格架主体特点

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张允平, 宋维民, 那福超, 鲍庆中, 汪岩. 东北亚活动大陆边缘中生代构造格架主体特点[J]. 地质与资源, 2016, 25(5): 407-423. doi: 10.13686/j.cnki.dzyzy.2016.05.001
引用本文: 张允平, 宋维民, 那福超, 鲍庆中, 汪岩. 东北亚活动大陆边缘中生代构造格架主体特点[J]. 地质与资源, 2016, 25(5): 407-423. doi: 10.13686/j.cnki.dzyzy.2016.05.001
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ZHANG Yun-ping, SONG Wei-min, NA Fu-chao, BAO Qing-zhong, WANG Yan. CHARACTERISTICS OF THE TECTONIC FRAMEWORK OF NORTHEAST ASIAN MESOZOIC ACTIVE CONTINENTAL MARGIN[J]. Geology and Resources, 2016, 25(5): 407-423. doi: 10.13686/j.cnki.dzyzy.2016.05.001
Citation: ZHANG Yun-ping, SONG Wei-min, NA Fu-chao, BAO Qing-zhong, WANG Yan. CHARACTERISTICS OF THE TECTONIC FRAMEWORK OF NORTHEAST ASIAN MESOZOIC ACTIVE CONTINENTAL MARGIN[J]. Geology and Resources, 2016, 25(5): 407-423. doi: 10.13686/j.cnki.dzyzy.2016.05.001
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东北亚活动大陆边缘中生代构造格架主体特点

  • 1.

    中国地质调查局 沈阳地质调查中心(沈阳地质矿产研究所), 辽宁 沈阳 110034;

  • 2.

    中国地质调查局 发展研究中心, 北京 100037;

  • 3.

    东北大学 研究生院, 辽宁 沈阳 110004

详细信息
    作者简介: 张允平(1951-),男,研究员,主要从事大地构造、区域地质与区域成矿规律研究,通信地址 辽宁省沈阳市皇姑区黄河北大街280号,Email//syzhyp@qq.com

  • 中图分类号: P541

CHARACTERISTICS OF THE TECTONIC FRAMEWORK OF NORTHEAST ASIAN MESOZOIC ACTIVE CONTINENTAL MARGIN

  • 1.

    Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China;

  • 2.

    Development and Research Center, CGS, Beijing 100037, China;

  • 3.

    Graduate School, Northeastern University, Shenyang 110004, China

    摘要
  • 东北亚是全球板块构造活动最复杂地区之一.中生代活动大陆边缘构造格架主体特点是，东部为陆缘增生带，包含碰撞造山带和增生造山带两种类型；西部为陆缘活化带，包含西伯利亚古陆东部活化区（北段），东蒙古-兴安-吉黑活化区（中段）和中-朝古陆东部活化区（南段）.整体构造格架具有东西分带，南北分段，由北东向南逐渐发展的特点.华北-蒙古-兴安地区中侏罗晚期-早白垩世初的沉积-火山-沉积磨拉石，属东北亚中生代活动大陆边缘构造演历进程的组成部分，是构造体制转换的标志之一.
    Northeast Asia is one of the most complex areas of plate tectonic activities in the world. The eastern continental margin accretion zone involves two types, i.e., collisional orogenic belt and accretionary orogen belt. The western margin reactivation zone contains Eastern Siberia ancient land reactivation region (north), East Mongolia-Xing'an-Jihei reactivation region (middle), and eastern Sino-Korea ancient land reactivation region (south). The overall structural framework of the Northeastern Asian Mesozoic active continental margin is characterized by zonation from east to west, segments from north to south, and development from northeast to south. The late Middle Jurassic-early Early Cretaceous sedimentary-volcanic-sedimentary molasse in North China-Mongolia-Xing'an Region, which is a component part of the Northeast Asian Mesozoic activite continental margin in its evolutionary process, is one of the indicators of tectonic system transition.
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出版历程
收稿日期:  2016-07-08
刊出日期:  2016-10-31

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