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核幔边界(古氏不连续面)是地核地函的交界。

1914年,德国地球物理学宾诺·古登堡Beno Gutenberg)发现地下2885千米地震波的传播速度有明显变化,其中纵波的速度明显下降,横波完全消失。后来证实这里是地核地幔的分界层[1]

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