A mineral assemblage of sulfides and sulfo-arsenides from the ophiolite mantle in Tibet;
来自蛇绿岩地幔的硫(砷)化物矿物组合
Water content in the Earth s mantle .;
地幔中水的存在形式和含水量
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
This paper gives a comprehensive review of studies on oxygen fugacity of the Earth mantle.
通过对目前国际上诸多有关地幔氧逸度的研究结果的系统分析和总结 ,提出了地幔中自由氧对地幔物质的性质、状态及运动过程产生影响的基本作用方式 ;介绍了目前地幔氧逸度研究的主要研究手段 ,包括本征氧逸度的实验室测量、模拟氧逸度的实验室测量、地幔氧逸度计及理论计算等及其优缺点 ;定性探讨了地幔氧逸度的时空分布规律 ,获得了地幔随时间的推移变得愈来愈氧化 ,随深度的增加变得愈来愈还原 ,以及在横向上不同大地构造部位的地幔区域具有不同的氧逸度等诸多结论。
The ore-forming materials are mainly derived from the earth core constrained by deep processes and moved up to surface with multi-stages of mantle plume evolution and is contaminated with earth crust materials.
认为峪耳崖矿区成矿物质应主要来自地核,受深部过程的约束,成矿物质随地幔热柱多级演化向地表迁移,在其上升过程中,与壳源物质发生部分混染,使所测同位素数据往往表现出以深源为主、并混有少量壳源物质的特征。
Mantle branch is the third-grade tectonic unit during multiple evolution of mantle plume.
幔枝构造是地幔热柱多级演化的三级单元,其对内生矿产的成矿控矿作用十分明显。
Mantle branch structure is the third-order unit of mantle plume multistage evolution.
幔枝构造是地幔热柱多级演化的第三级构造单元 ,其核部变质—岩浆杂岩隆起与外围盖层之间的主拆离带体系是很好的成矿控矿构造。
Progress in the research on noble gas isotope tracing of the mantle plume and its significance.;
地幔柱稀有气体同位素示踪研究的进展及其意义
Petrogenesis of the basalts of Woniusi Formation at Baoshan area, Yunnan: Is it of mantle plume origin?;
云南保山卧牛寺组玄武岩成因:地幔柱活动的产物?
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。
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。
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
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。
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。
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.
Like the core of earth, the mantle can also be pided 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。
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。
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
An upwelling of molten material from the earth's mantle.
地柱从地幔隆起的一段熔化物
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
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
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。
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。
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。
PRELIMINARY STUDY ON THE LATERAL VELOCITY VARIATION OF THE UPPER MANTLE IN NORTHERN XINJIANG AND ITS ADJOINING REGIONS
北疆上地幔波速特征侧向变化的探讨
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
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