embryonic mantle layer 胚胎外膜层
crust-mantle transition layer 壳幔过渡层
upper mantle conductivity layer 上地幔高导层
crust-mantle transitional layer 壳幔过渡层
two layer mantle model 双层地幔模式
The lowermost mantle layer is above the core mantle boundary (CMB) and composed of D" region and ultra-low velocity zone (ULVZ)."
地幔底层由具有高地震波速和高密度的D″区和超低速带(ULVZ)组成。
Surprisingly, precious metals instead appear relatively abundant on the planet's surface and in the underlying mantle layer. [Infographic: Tallest Mountain to Deepest Ocean Trench].
令人惊讶的是,在地球表面和下面的地幔层里贵金属反而比较丰富。
All are slowly moving because the plates float on a denser sem-iliquid mantle, the layer between the crust and Earth's core.
所有板块都在缓慢移动,因为它们漂浮在密度更大的半流体地幔上,也就是地壳和地核之间的那一层。
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