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地幔底部與地核外層的不連續性交匯處 来自维基百科,自由的百科全书
1914年,德国地球物理学家宾诺·古登堡(Beno Gutenberg)发现地下2885千米处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与地幔的分界层[1]。
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