1) core-mantle boundary
地核-地幔边界
2) core-mantle boundary
核-幔边界
1.
The core-mantle boundary (CMB ) is the greatest contrasting and the most important boundary in the interior of Earth, where core-mantle interactions have been playing an important role in earth s geodynamics system.
核-幔边界是地球内部反差最大的一个边界，也是最重要的边界。
3) core-mantle boundary
核幔边界
1.
The latest global mantle seismic tomographic data have revealed tectonics beneath plates:the lithospheric slab may be subducted to the core-mantle boundary and the superplume may rise from the core-mantle boundary to the upper crust to form a hot spot.
最新的全球地幔地震层析资料揭示了岩石圈板片可以俯冲到核幔边界,超地幔羽可以从核幔边界上升到地壳上部形成热点。
4) core boundary
地核边界
5) Core-mantle boundary (CMB) topography
核幔边界(CMB)起伏
6) crust-mantle boundary
地壳-地幔边境
补充资料：地核
| 地核 earth core 地球的核心部分。主要由铁、镍元素组成，半径为3480千米。地核又分为外地核和内地核两部分。外地核的物质为液态。见地球内部构造。 |
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参考词条