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. 地球系统多圈层构造观的基本内涵[J]. 地质力学学报, 2019, 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, 徐芹芹, 朱俊宾. 地球系统多圈层构造观的基本内涵[J]. 地质力学学报, 2019, 25(5): 607-612. doi: 10.12090/j.issn.1006-6616.2019.25.05.058
REN Jishun, NIU Baogui, ZHAO Lei, XU Qinqin, ZHU Junbin. BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM[J]. Journal of Geomechanics, 2019, 25(5): 607-612. doi: 10.12090/j.issn.1006-6616.2019.25.05.058
Citation: REN Jishun, NIU Baogui, ZHAO Lei, XU Qinqin, ZHU Junbin. BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM[J]. Journal of Geomechanics, 2019, 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

  • 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

  • 责任编辑:吴芳

BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM

  • 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。

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  • 图 1  大地构造理论发展历程

    Figure 1. 

    图 2  现今地球大地水准面图(马宗晋先生提供)

    Figure 2. 

    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. 

    图 4  西伯利亚克拉通地震速度剖面(据文献[17]重绘)

    Figure 4. 

    图 5  全球板块构造简图(据文献[11, 23]重绘)

    Figure 5. 

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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:  2019-10-31

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