1.
Plumes are generally believed to form over localized hot spots deep within the mantle layer.
地慢羽一般被认为是形成于地幔层内部深处固定的热点上。
2.
Therefore, the CMB is the beginning and the end of whole mantle convection.
因此,地幔底层既是全地幔对流的起点,又是全地幔对流的终点。
3.
Like the core of earth, the mantle can also be divided into two concentric layers, the lower mantle and the upper mantle.
就像地球的核部一样。地幔也可分为两个同心圆圈层，下地幔和上地幔。
4.
Surface Wave Tomography of the Crust and upper Mantle in Sichuan-Yunnan Region;
川滇地区地壳及上地幔结构面波层析成像
5.
Scientists call this layer of crust and upper mantle the lithosphere.
科学家称这层地壳和上部地幔为岩石圈。
6.
A Seismic Tomography Study on Crust and Upper-mantle Structure Beneath the North-South Zone in China;
南北带地壳上地幔结构的层析成像研究
7.
Surface Wave Tomography in China and Adjacent Areas;
中国及邻区地壳上地幔面波频散层析成像
8.
Like the earth, the moon is in layers, with a crust on the outside and a deep mantle below.
如同地球一样，月球上有地层，表面是一层地壳，其下是很深的地幔。
9.
Each plate consists of a section of the earth's crust and a portion of the mantle, the thick layer of hot rock below the crust.
每个板块由一段地壳和一部分地壳下部厚层炽热岩石地幔组成。
10.
The Seismic Tomography on the Velocity Structure of the Crust and Upper Mantle in the Northeastern Margin of the Qinghai-Tibetn Plateau
青藏高原东北缘地壳上地幔速度结构的地震层析成像研究
11.
The plates move slowly and continuously on the atmosphere, a layer of hot, soft rock in the mantle.
板块缓慢连续地在软流圈上移动，该软流圈是指地幔中炽热柔软层。
12.
Tomography for The 3-D S -Wave Quality Factor Q_B Structure of Crust and Upper Mantle in China;
中国大陆地壳上地幔S波品质因子三维层析成像
13.
The 3-D velocity structures of the Eurasian mantle based on the body wave tomography
利用体波层析成像技术研究欧亚及邻区地幔三维速度结构
14.
Tomography for the 3-D S-Wave Quality Factor Q_β Structure of Crust and upper Mantle in China and Adjacent Areas;
中国大陆及邻区上地幔S波品质因子三维层析成像
15.
High Resolution Body-Wave 3-D Tomography of Mantle of China and Adjacent Areas;
中国及邻区地幔三维结构高分辨率体波层析成像
16.
Upper Mantle Structure Beneath the Chinese Capital Region from Teleseismic Finite-frequency Tomography
应用远震有限频率层析成像反演首都圈上地幔速度结构
17.
An ornamental hanging of rich fabric, as behind an altar.
幔布祭坛后面等地的幔布
18.
In east pacific, however, the subduction direction of the subducting plate is the same as that of the flow of the mantle, so the current dip angle of the Benioff zone will be larger than the initial dip angle.
对地幔而言 ,则是地幔相对于地壳的东向流动。