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    岩浆作用与地球深部过程

    莫宣学

    莫宣学, 2019. 岩浆作用与地球深部过程. 地球科学, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972
    引用本文: 莫宣学, 2019. 岩浆作用与地球深部过程. 地球科学, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972
    Mo Xuanxue, 2019. Magmatism and Deep Geological Process. Earth Science, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972
    Citation: Mo Xuanxue, 2019. Magmatism and Deep Geological Process. Earth Science, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972

    岩浆作用与地球深部过程

    doi: 10.3799/dqkx.2019.972
    详细信息
      作者简介:

      莫宣学(1938-), 男, 教授, 中国科学院院士, 学科专业为岩石学, 研究方向为岩浆-构造-成矿

    • 中图分类号: P54

    Magmatism and Deep Geological Process

    • 摘要: 为纪念马杏垣院士诞辰一百周年而作.首先简述了地球系统科学的基本思想和指导意义.指出岩浆作用实质上是地球各层圈之间相互作用的结果,岩浆是地球各层圈之间物质和能量交换的重要载体.通过众多研究实例,重点讨论了岩浆作用的地球动力学意义:一方面,火成岩及其所携带的深源岩石包体可以当作地球深部的"探针"和"窗口";另一方面,火成岩也是大地构造事件的记录,可以用以恢复古板块构造格局,追溯大地构造演化历史.

       

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    • 刊出日期:  2019-05-15

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