1) core-mantle mill
核-幔磨
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 coupling
核幔耦合
1.
Tentative researche s demonstrate that: core-mantle coupling induced fluctuations in crustal deform ation, geophysical observations, are important modulations to back-ground anoma ly variations on years to decad.
初步分析表明深部核幔耦合作用引起的地壳形变、地球物理场十年尺度波动,是数年至十年尺度地震场兆波动性变化的重要调制因素之一;源于断层脆韧转换带(过渡层)的静寂地震慢地震缓慢破裂过程,是数天至数月尺度地震短期异常变化产生的重要原因;源于脆韧转换层上部或弹脆性层薄弱部分慢地震过程所辐射出来的低频前驱波(慢地震波),是目前已发现的可重复出现的短临前兆信号,具有数小时至7天左右的地震短临预报指标意义。
2.
Three possible core-mantle coupling mechanisms, topographic coupling, electromagnetic coupling and gravitational coupling, have been proposed, but no one was thoroughly, verified or ruled out.
已提出了三种可能的核幔耦合机理即核幔地形耦合、电磁耦合、引力耦合，但至今没有一个被完全证实或排除。
4) different speed rotation of the inner core and the mantle
核幔转差
5) 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。
6) earth's core-mande body
核幔体
补充资料：磨核
1.仔细查对。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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