In 1906 a British geologist discovered that P waves slowed down at a certain depth but kept traveling deeper. On the other hand, S waves either disappeared or were reflected back, so he concluded that depth marked the boundary between a solid mantle and a liquid core核心, 精髓, 要点. Three years later another boundary was discovered that between the mantle and the Earth's crust
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) @, v1 D6 L8 j% W1 e在1906年有位英国地质学家发现P波到一定深度后虽然可以继续下行速度却下降了,而s波要么消失要么被返回了,因而他总结出在那个深度的固体地幔和液体核心之间有个边界。三年之后在地幔和地壳之间发现了另一个边界。
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2 |; N9 e/ @0 I, S3 B4 w! z* }$ sPS:达达,你是具体那句不理解吧,也没说清楚,就拿整段的整段的折磨我们
