热柱

本研究的结果表明，在中太平洋的地幔底部存在着大范围的AB-DF走时正残差，也即低速异常区，这可能是太平洋下超大地幔热柱的源处。

Our results show large positive AB-DF differential time residuals across large areas of the lowermost mantle beneath the central Pacific , which may indicate the source region of the " Pacific Super Plume " .

初论地幔热柱与铀成矿的关系

Discussion of the relationship between mantle plume and uranium mineralization

结果表明，与同等尺寸下的铜柱散热器相比较，在相同工况条件下，热柱散热器能带走更多的热量，使CPU的表面温度降的更低，并且对CPU热源具有良好的均热效果。

The results show that compared with the same size copper pillar radiator , the thermal column radiator can drop the temperature of CPU lower , and has a good soaking effect on the CPU heat source .

由于热柱孔道内有一个50cm长的硅过滤器，所以中子能谱偏离典型的麦克斯韦分布。

The result shows that the neutron energy spectrum is quite different from a typical Maxwell distribution . This is because that there is a silicon filter of 50 cm long inside the hole of the thermal column .

基于虚拟仪器的热柱体旋涡脱落特性实验研究

Experimental Research Based on Virtual Instrument for Vortex-shedding Characteristics of Heated-cylinder

核幔成矿物质（流体）的反重力迁移&地幔热柱多级演化成矿作用

The anti - gravity migration of metallogenic fluid from core and mantle

重水反应堆热柱中子能谱测量

Measurement of neutron energy spectrum at thermal column of heavy water reactor

霍特导弹包装地幔热柱及其成矿作用研究

The Packaging of " Hot " Missile Mantle Plume and its Mineralization

热柱起源以及巨大热柱附近地区地幔结构的地震学研究介绍

Introduction of seismological study for plume origin and mantle structure near large plume

水平液体绕流热柱体旋涡脱落特性的研究

Study on the Vortex Shedding Characteristics in Horizontal Flow around Heated Circular Cylinder

试论华北地台中生代超变质作用与地幔热柱作用

Mesozoic Ultra-metamorphism and Mantle Plume in North China Platform

地幔热柱成矿作用研究进展

Research advance in mineralization of mantle plumes

这一结果有助于太平洋下超大地幔热柱的结构和性质的进一步研究。

The results have implications for understanding the structure and nature of the Pacific Super Plume .

氮氧化物羽烟在电离层局部的光热效应地幔热柱及其成矿作用研究

OPTICAL - THERMAL EFFECT OF NO_x EXHAUST PLUME IN LOCAL IONOSPHERE Mantle Plume and its Mineralization

飞行时间法测量脉冲堆热柱孔道热中子能谱

Thermal Neutron Spectrum in Thermal Column of Pulse Reactor Measured Techniques With Time of Flight Method

地幔热柱演化及其地热效应&华北地热异常的深部构造背景

The Mantle Plume Evolution and Its Geothermal Effect & Deep Tectonic Setting of Geothermal Anomaly in North China

地幔底层既是俯冲板块的最终归宿，又是热柱和超级热柱的源区。

The CMB is the impinged by subducted slAbs and is the source of mantle plumes and super plumes .

以中国为例，研究了幔柱构造特征，提出了地幔热柱构造的动力学模型。

Finally , taking China as an example , we study the behavior of mantal pillar tectonics in the mantle .

它的形成与特殊的地幔动力作用过程&峨眉地幔热柱活动有关。

Its formation is concerned with the product of a unique mantle dynamic process , i.e. the Emei mantle plume activity .

并推导出热柱散热器的总传热模型，找出了影响散热的关键因素。

And we derive the total thermal column radiator heat transfer model ; find the key factors affecting the heat transfer .

游泳池反应堆热柱中子束空间分布、能谱及剂量参数的测定

The determination of the space distribution , energy spectrum and dose parameter of thermal column beam resulting from swimming pool reactor

最后，从地幔热柱的多级演化角度，结合本研究区的实际地质情况，绘制了铜成矿模式图。

Lastly , based on the actual geological condition and view of multistage evolution of mantle plume , this paper establishes the metallogenic model of copper .

通过对黔西南卡林型金矿床形成特殊性研究，显示：黔西南金矿位于特殊的大地构造位置；峨眉地幔热柱活动对该区构造、岩浆活动产生极大影响；

A study on forming particularity of Carlin-type gold deposits in southwestern Guizhou Province shows that southwestern Guizhou Province belongs to a particular part in tectonics ;

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。

The main detachment zone system between metamorphic magmatic complex uplift and cover of the periphery of the mantle branch is good for ore-forming and ore-controlling structures .

同时，搭建了实验测试装置，对热柱散热器进行了测试实验，研究其在不同工况下散热器的散热性能。

At the same time , the experimental device is manufactured which is used to test thermal column radiator and study its performance under different operating conditions .

柴达木第三纪转换裂陷盆地形成演化主要受控于地幔热柱的形成和衰减作用，同时喜马拉雅运动等运程应力作用对盆地的演化至关重要。

The formation and evolution of the basin are considered to be constrained by the formation and waning of mantle plumes and stress processes of the Himalayan orogeny .

这一复合低速柱反映了峨眉山地幔热柱的纵向与横向不均匀性和多级演化特征。

The occurrence of this composite low-velocity plume reflects the heterogeneity of the Emei mantle plume in both vertical and lateral directions and the characteristics of its multi-stage evolution .

基于本文的叠加方法，我们可以快速准确地得到地下间断面的起伏，并与物质的温度异常联系起来，从而可以用来探测地球内部俯冲板块和热点热柱的分布。

Based on the upper method , we can obtain the topography of the discontinuities immediately , which is correlated with the distribution of the subducted slab and hotspots and plume .

在地幔热柱多级演化过程中，特别是在通过地幔进入地壳后，不可避免地会融入部分壳源物质，这就使得所测数据往往介于典型幔源区与壳源区之间。

During the multi-stage evolution of mantle plume , especially the ore-forming materials found their way into the crust vias the mantle , it is inevitable that some crustal material would have been involved .

分析了形成上述地球物理特征的3种因素：东亚大陆边缘周边三大板块运动、地幔流运动和地幔热柱。

We analyses 3 kinds of factors to generate the above-mentioned geophysical characteristics , such as the mantle current movement , the mantle thermal plume and the three plates movement surrounding around the continental margin .