1.
Experimental Study on the Electrical Conductivity of Mantle Minerals at High Temperatures and High Pressures
地幔矿物电导率的高温高压实验研究
2.
The mantle mineral group in Tibet has great significance in mineralogy an d geodynamics.
西藏地幔矿物群,无论在矿物学和地球动力学上均有重要意义。
3.
Experimental Study on Electrical Conductivities of upper Mantle Minerals and Rocks under High Temperature, High Pressure, and Different Oxygen Fugacity Conditions;
高温高压和不同氧逸度下上地幔矿物岩石电导率的实验研究
4.
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
5.
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
6.
Simulates on Melting, Elastic and Thermodynamic Properties of Major Material of the Lower Mantle;
下地幔主要矿物的熔化、弹性和热力学特性研究
7.
As the subducting plate is heated back up to mantle temperatures, certain minerals in the plate melt sooner than others.
随着俯冲板块被加热而回升到地幔的温度，板块中的某些矿物较其他矿物先熔化了。
8.
The eruptions have changed the environment, and also formed the important resources of minerals, geotherm and touring.
它把地幔和地壳物质喷出地表，改变和影响环境，同时形成重要的矿产、热和旅游等资源。
9.
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
10.
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
11.
Mineral Chemistry of Peridotitic Xenoliths in Yangyuan Cenozoic Basalts: Significance for Lithospheric Mantle Evolution Beneath the Trans-North China Orogen
河北阳原新生代玄武岩中橄榄岩捕虏体矿物化学特征：华北内部山带岩石圈地幔演化意义
12.
Mineral Chemistry of Peridotite Xenoliths in Yangyuan Cenozoic Basalts:Significance for Lithospheric Mantle Evolution beneath the North China Craton
河北阳原新生代玄武岩中橄榄岩捕虏体矿物化学:华北岩石圈地幔演化
13.
An upwelling of molten material from the earth's mantle.
地柱从地幔隆起的一段熔化物
14.
Advances in the Structure and Stability of Perovskite under Deep Mantle;
下地幔钙钛矿顽火辉石相稳定性研究及其进展
15.
Preliminary Discussion of the Relation Between Mantle Plume Structure of Emei Mountain and Uranium Mineralization of Guizhou
峨眉山地幔柱构造与贵州铀成矿关系初探
16.
Stability of(Mg,Fe)SiO_3-Perovskite under the Condition of Lower Mantle Pressure and Temperature
下地幔温压下(Mg,Fe)SiO_3钙钛矿的相稳定性
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.
Evidence indicates that the outer core is about twice as dense as the material in the mantle.
有证据表明，外地核的密度约为地幔物质的两倍。