1.
PETROLOGY AND MINERALOGY OF PERIDOTITES FROM THE SOUTHERN MARIANA FOREARC:IMPLICATION FOR THE METASOMATISM OF THE MANTLE WEDGE UNDER MARIANA ARC
马里亚纳南部前弧橄榄岩的岩石及矿物学:对弧下地幔楔交代作用的指示
2.
Upward mantle wedge convection recorded by Zhimafang orogenic garnet-lherzolite,Sulu UHP terrane,eastern China.
洋壳俯冲过程中的地幔楔上升对流:来自芝麻坊石榴子石二辉橄榄岩早期变质的证据
3.
An ornamental hanging of rich fabric, as behind an altar.
幔布祭坛后面等地的幔布
4.
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。
5.
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。
6.
New seismic constraints on the upper mantle structure of the Hainan plume
海南地幔柱上地幔结构新的地震学约束
7.
The issue of upper vs whole mantle convection is critically discussed.
最后,着重讨论了上地幔与全地幔对流的论争。
8.
Contrast research of bearing characteristic for composite foundation with tapered piles and cylindrical piles
楔形刚性桩复合地基中桩的最佳楔角范围研究
9.
The earth have a core and a mantle around it.
地球的中心是地核，地核的周围是地幔。
10.
The earth has a core and a mantle around it.
地球的中心是地核, 地核的周围是地幔.
11.
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。
12.
There is a higher heat production in the upper mantle below oceans than below continents.
大洋下的上地幔要比大陆下的上地幔有较高的热产率。
13.
ROUNDED MINERAL INCLUSIONS IN XENOLITHS FROM SOME AR EAS OF EASTERN CHINA AND THEIR BEARING ON THE ANNEALING TIME OF MANTLE PERIDOTITES
我国东部某些地幔岩中圆形矿物包裹体及地幔岩退火时间的探讨
14.
An upwelling of molten material from the earth's mantle.
地柱从地幔隆起的一段熔化物
15.
Variable Viscosity Whole Mantle Convection and Surface Plate Motions;
全球变粘度地幔对流与地表板块运动
16.
Mineralogical Deduction of Characteristics of the Mantle Beneath North Hetian Area;
和田地区北部地幔特征的矿物学反演
17.
The upwelling of the mantal substance along fractured zones may be the reason causing the abnormal crust and mantal structure.
地幔物质沿断裂带上涌，可能是形成异常壳幔结构的原因。
18.
Plumes are hot enough to melt their way through the ocean floor or through a continent.
地幔羽的热量足以熔穿海底或大陆。