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What Lies Beneath THE FORMATION AND EVOLUTION OF OCEANIC LITHOSPHERE

机译:海洋岩石球的形成和演化背后的原因

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摘要

Sampling the upper mantle via scientific ocean drilling remains elusive. Although the technologies required for drilling to the Moho still don't exist, we have made significant progress over the last five decades in piecing together the complex geology of the oceanic crust. Here, we highlight key findings that reveal the architecture of oceanic crust and the thermal, physical, and chemical processes that are responsible for the growth and structure of the oceanic lithosphere. These advances result from enduring efforts to drill and collect downhole geophysical logs of oceanic crust near both slow and fast spreading ridges.
机译:通过科学的海洋钻探对上地幔进行采样仍然很困难。尽管钻探Moho所需的技术仍然不存在,但在过去的五十年中,我们在将复杂的海洋地壳地质学拼凑起来方面取得了重大进展。在这里,我们重点介绍了揭示洋壳结构以及热,物理和化学过程的重要发现,这些洋壳构成了海洋岩石圈的生长和结构。这些进展源于长期努力在缓慢和快速扩张的山脊附近钻探和收集海底地壳地球物理记录。

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  • 来源
    《Oceanography》 |2019年第1期|138-149|共12页
  • 作者单位

    Nagoya Univ, Grad Sch Environm Studies, Dept Earth & Planetary Sci, Nagoya, Aichi, Japan;

    Woods Hole Oceanog Inst, Natl Deep Submergence Facil, Woods Hole, MA 02543 USA;

    Univ Montpellier, CNRS, Geosci Montpellier, Res, Montpellier, France;

    Univ Southampton, Natl Oceanog Ctr Southampton, Sch Ocean & Earth Sci, Southampton, Hants, England;

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