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    星地碰撞的板块构造效应

    刘广润 张宏泰 唐辉明

    刘广润, 张宏泰, 唐辉明, 2007. 星地碰撞的板块构造效应. 地球科学, 32(3): 381-388.
    引用本文: 刘广润, 张宏泰, 唐辉明, 2007. 星地碰撞的板块构造效应. 地球科学, 32(3): 381-388.
    LIU Guang-run, ZHANG Hong-tai, TANG Hui-ming, 2007. The Effect of the Impact of a Celestial Body with the Earth on the Plate Structure of the Crust. Earth Science, 32(3): 381-388.
    Citation: LIU Guang-run, ZHANG Hong-tai, TANG Hui-ming, 2007. The Effect of the Impact of a Celestial Body with the Earth on the Plate Structure of the Crust. Earth Science, 32(3): 381-388.

    星地碰撞的板块构造效应

    详细信息
      作者简介:

      刘广润(1929-), 男, 中国工程院院士, 主要从事工程地质环境地质研究.E-mail: liugrs@tom.com

    • 中图分类号: P541

    The Effect of the Impact of a Celestial Body with the Earth on the Plate Structure of the Crust

    • 摘要: 板块构造是一种全球大地构造理论.它以洋底扩张、洋壳边缘俯冲及转换断层为主要构造活动形式, 配以地幔对流为原动力, 建立一套颇具魅力的板块构造机制理论, 被受到广泛认同.但也存在一些重要问题, 主要是其地幔对流理念难以令人信服和对海陆格局变迁问题没提出明确的动力机制.在阐明造成板块构造理论这两方面困难问题的主要理由之后, 介绍了星地碰撞事件的存在状况及其动力作用, 着重论述了大规模星地碰撞的动力作用强大, 对全球地质构造活动都有重要影响, 板块构造也难以避免; 星地碰撞的强烈冲击作用, 有能力造成洋底开裂或使大陆裂解.据此设想, 可用“星地撞击成缝, 减压诱发岩浆上侵”的模式, 取代与地球内部层圈结构相抵触的“地幔对流”模式来解释洋底扩张; 并以星地碰撞发生地点的随机变化性作为大规模海陆格局变迁的主控原因.如此, 则可有助于上述板块构造理论中存在的两大难题的解决.

       

    • 图  1  全球板块构造分区图(转引自上田诚也, 1973)

      1.扩张轴, 大洋裂谷; 2.洋壳俯冲到大陆架之下; 3.几种类型的断裂带; 4.大陆裂谷; 5.洋壳俯冲到科迪勒拉山系之下; 6.洋壳俯冲到洋壳之下; 7.大陆-大陆碰撞

      Fig.  1.  Distribution of global plate tectonics

      图  2  地幔对流及洋底扩张示意剖面图(a图和b图转陈琦和刘永祥, 2004; c图据鄢全树和石学法, 2006)

      Fig.  2.  Schematic section of mantle convection and sea-floor spreading

      图  3  地球内部层圈结构划分图(a)、地球内部圈层的波速和密度图(b)和地球内部圈层物理数据统计(c)

      Fig.  3.  Distribution of layers in earth interior (a); Map of wave velocity and density of layers in earth interior (b); Statistics of physical data of layers in earth interior (c)

      图  4  南非维德佛特陨石坑卫片图像

      Fig.  4.  Satellite image of Vredefort aerolite pit in South Africa

      图  5  星地碰撞的动力作用图解

      Fig.  5.  Map of dynamic action of collision of a celestial body with the earth

      表  1  地震震级与地震裂缝长度的关系统计

      Table  1.   Statistics of seismic magnitude and the length of seismic crack

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