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Beneath the Moon's Two Faces

机译:在月亮的两张脸下

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摘要

Astronomers have finally figured out why the moon is so two-faced, and it turns out the answer was with us all along: It's Earth's fault. The moon's two faces look nothing alike. The far side has significantly fewer of the familiar dark patches, formed by ancient lava flows. That's because the lunar crust is thicker there, making it harder for asteroid impacts to break through and release magma. But why was the crust thicker to begin with? A team of Pennsylvania State University astronomers came up with a likely answer last summer, one that dates back to the moon's formation. When a Mars-size body collided with the young Earth some 4.5 billion years ago, the material that shot into orbit eventually coalesced and cooled into the solid moon, with one side always facing Earth. But the crash also heated our planet to over 7,000 degrees Celsius (13,000 degrees Fahrenheit), energy that irradiated the moon's near side, keeping it molten much longer.
机译:天文学家们终于弄清楚了为什么月亮如此两面,结果答案一直伴随着我们:这是地球的错。月亮的两张脸看起来完全不一样。远侧具有较少的由古老熔岩流形成的熟悉的深色斑块。那是因为月球地壳在那里较厚,这使得小行星撞击很难突破并释放出岩浆。但是,为什么外壳开始变厚呢?宾夕法尼亚州立大学的一个天文学家小组在去年夏天提出了一个可能的答案,这个答案可以追溯到月球的形成。大约45亿年前,当一个火星大小的物体与年轻的地球相撞时,射入轨道的物质最终会聚结并冷却成固体的月球,一侧始终面向地球。但是坠机事件还把我们的星球加热到了7,000摄氏度(13,000华氏度)以上,这种能量辐射到了月球的近侧,使它融化了更长的时间。

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  • 来源
    《Discover》 |2015年第1期|61-61|共1页
  • 作者

    KATHERINE KORNEI;

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