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Earth's billion-year youthful rampage

机译:地球的十亿年青春狂潮

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摘要

Our planet has calmed down in its middle age. Earth was at its most active 1.1 billion years ago, when all the continents collided into one huge supercontinent, and has been getting calmer ever since. It's evidence that the planet has a kind of lifespan. Earth's surface layer, the crust, is divided into tectonic plates that constantly Jostle against each other. When two plates collide, they can be forced up into mountains, or one plate can slide under another and be destroyed. This tectonic activity has been going on for at least 3 billion years, but nobody knows whether Earth has been getting more or less active over time. To find out, Martin Van Kranendonk of the University of New South Wales and Christopher Kirkland of the Geological Survey of Western Australia set out to reconstruct the history of plate tectonics.
机译:我们的星球在中世纪已经平静下来。地球是11亿年前最活跃的时期,当时所有大洲都碰撞成一个巨大的超大陆,并且此后一直变得平静。有证据表明,行星具有某种寿命。地球的表层,地壳,被划分为不断相互碰撞的构造板块。当两个板块发生碰撞时,它们可能会被迫上山,或者一个板块会滑到另一个板块下面并被破坏。这种构造活动已经持续了至少30亿年,但是没有人知道地球是否随着时间的推移变得越来越活跃。为了找到答案,新南威尔士大学的马丁·范·克兰嫩东克和西澳大利亚州地质调查局的克里斯托弗·柯克兰德着手重建板块构造的历史。

著录项

  • 来源
    《New scientist》 |2013年第2916期|12-12|共1页
  • 作者

    Michael Marshall;

  • 作者单位
  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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