1.
HELIUM ISOTOPIC EVIDENCE ON METALGENISIS OF MANTLE FLUIDS IN THE WANGU GOLD DEPOSIT, HUN AN PROVINCE
湖南万古金矿床地幔流体成矿的氦同位素证据
2.
The Petrographic and Petrochemical Characteristics of the Mantle Fluid Metasomatism;
地幔流体交代作用的岩相学和岩石化学特征
3.
The Concentration Mechanism of Gold in the Crude Oil from Jiyang Depression and Its Relationship with the Mantle Fluid;
济阳坳陷原油中金的富集机理及其与地幔流体的关系
4.
Mantle fluid metasomatism in Jinhe intrusive body of Jianchuan,Yunnan Province,and its ore-forming implication
云南剑川金河岩体中地幔流体交代特征及其成矿意义
5.
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。
6.
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。
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.
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
9.
Numerical experiment is a basic method in the study of Earth's mantle convection.
数值实验是地幔对流研究的基本方法。
10.
Numerical Modeling of upper Mantle Convection and Orogeny of the Tianshan Mountains;
天山上地幔对流与造山运动数值模拟
11.
Temporal Variation in Volume Flux of Hawaii Plume through 35 Ma
Hawaii地幔柱近35Ma的体积流量变化
12.
The Geological Evolution and Mantle Convection of the North China Platform in Early Precambrian
华北陆台早前寒武纪地质演化与地幔对流模式
13.
The mesosphere comprises the rest of the mantle below the asthenosphere.
中间圈包括岩流圈以下地幔的其余部分。
14.
The Chemical and Isotopic Compositions and Their Origin of Upper Mantle Volatiles in Eastern China;
中国东部上地幔不同类型流体组成及其性质
15.
The Numerical Modelling of Whole Mantle Convection and Its Geodynamic Implications;
全球地幔对流的数值模拟及其动力学意义
16.
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。
17.
Siberian clod downwelling is from surface dive to near CMB;
西伯利亚下降流，规模大，从地表下降到下地幔下部；
18.
Recycled Crustal Volatiles in the Subcontinental Lithospheric Mantle beneath Eastern China
中国东部陆下岩石圈地幔中的再循环地壳流体组分