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地球系统多圈层构造观的基本内涵

任纪舜 牛宝贵 赵磊 徐芹芹 朱俊宾

任纪舜, 牛宝贵, 赵磊, 等, 2019. 地球系统多圈层构造观的基本内涵. 地质力学学报, 25 (5): 607-612. DOI: 10.12090/j.issn.1006-6616.2019.25.05.058
引用本文: 任纪舜, 牛宝贵, 赵磊, 等, 2019. 地球系统多圈层构造观的基本内涵. 地质力学学报, 25 (5): 607-612. DOI: 10.12090/j.issn.1006-6616.2019.25.05.058
REN Jishun, NIU Baogui, ZHAO Lei, et al., 2019. BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM. Journal of Geomechanics, 25 (5): 607-612. DOI: 10.12090/j.issn.1006-6616.2019.25.05.058
Citation: REN Jishun, NIU Baogui, ZHAO Lei, et al., 2019. BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM. Journal of Geomechanics, 25 (5): 607-612. DOI: 10.12090/j.issn.1006-6616.2019.25.05.058

地球系统多圈层构造观的基本内涵

doi: 10.12090/j.issn.1006-6616.2019.25.05.058
基金项目: 

中国地质调查项目 DD20190358

详细信息
    作者简介:

    任纪舜(1935-), 男, 研究员, 博士生导师, 中国科学院院士, 主要从事大地构造和区域地质研究。E-mail:renjishun@cags.ac.cn

  • 中图分类号: P54

BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM

  • 摘要: 地球系统多圈层构造观的基本点是,把地球作为一个活的天体放在宇宙系统之中,更多地考虑地球深部壳-幔-核之间的相互作用,考虑地外天体对地球运动的作用和影响。这一构造观认为:构造运动并不仅仅是岩石圈板块之间的相互作用,而是地球系统的全球动力作用过程;陆与洋是对立统一相互转化的,单纯的大陆增生说是不正确的;地幔对流说至今未被证实,陆块是活动的,但不能大规模漂移;大陆地壳不是单纯地侧向或垂向增生,而是多旋回构造-岩浆作用叠合的产物;地球的构造不是均变式向前发展,而是非均变、非线性、旋回式向前演化的;地球表层在不同地史阶段,均有其受相应深断裂体系控制的不同的构造格局,大西洋-印度洋-太平洋式大洋盆体制,只是在中生代晚期以来才出现的。

     

  • 图  1  大地构造理论发展历程

    Figure  1.  Development of the tectonic theory

    图  2  现今地球大地水准面图(马宗晋先生提供)

    图中清楚显示出东亚大陆的轮廓以及西太平洋沟-弧-盆体系

    Figure  2.  Geoid of the Earth (provided by MA Zongjin)

    图  3  横穿大西洋扬马延海台的地震剖面P波速度模型及地质解释[14]

    Figure  3.  The P-wave velocity model for the profile across the Jan Mayen Ridge and Jan Mayen Basin with geological interpretation[14]

    图  4  西伯利亚克拉通地震速度剖面(据文献[17]重绘)

    Figure  4.  Velocity cross-section along the Siberian Craton profile (redrawn after reference [17])

    图  5  全球板块构造简图(据文献[11, 23]重绘)

    Figure  5.  Major lithospheric plates of the globe (redrawn after references [11, 23])

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出版历程
  • 收稿日期:  2019-09-10
  • 修回日期:  2019-09-27
  • 刊出日期:  2019-10-28

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