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The proto-terrestrial mechanism of the appearance of water and early genesis of the global ocean

机译:水的出现和全球海洋早期成因的原地面机制

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摘要

We consider chemical reactions for the appearance of water during the formation of the planet from cosmic gas and dust material to explain the early geological existence of the Earth's hydrosphere. This process is fully supported by the resources of the initial substances and thermal energy. Thus, the concept of V.I. Vernadsly about the geological eternity of the World Ocean and ancient age of the oceanic lithosphere is supported. The identical high location of the ancient and modern continental platforms under the conditions of continual isostatical equilibrium in the asthenosphere-lithosphere-hydrosphere gives grounds to conclude that the ocean water depth is stable. Taking this into account, we can consider that the geological evolution of the Earth began in the conditions of the existence of the World Ocean when the mass of the hydrosphere only slightly exceeded the modern one.
机译:我们考虑由宇宙气体和尘埃物质在行星形成过程中对水的外观进行化学反应,以解释地球水圈的早期地质存在。初始物质和热能的资源完全支持该过程。因此,V.I。的概念全面支持世界海洋的地质永恒性和海洋岩石圈的古老时代。在软流圈-岩石圈-水圈连续等静压平衡的条件下,古代和现代大陆平台的高位相同,因此有理由得出结论,海洋水深是稳定的。考虑到这一点,我们可以认为地球的地质演化是在世界海洋存在的条件下开始的,当时水圈的质量仅略超过现代海洋。

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  • 来源
    《Doklady Earth Sciences》 |2016年第2期|892-894|共3页
  • 作者

    Sergin S. Ya;

  • 作者单位

    Russian Hydrometeorol Univ, Tuapse Branch, Ul Morskaya 4, Tuapse 352800, Krasnodar Krai, Russia;

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  • 正文语种 eng
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