mantle flow的例句大全

Undulation of Moho and Ductile Flow of Lower Crust Induced by Mantle Flow

地幔对流诱发的莫霍面起伏与下地壳塑性流动

present-day mantle flow and its interaction with plate tectonics inferred from observational evidence

现今的地幔流动及其与板块构造的相互作用：从观测证据得到的推论

interpretation of seismic anisotropy in terms of mantle flow when melt is present

当融化时根据覆盖层流动对地震各向异性的解释

a study of global vertical velocity of mantle flow

全球地幔垂直流动速度研究

mantle flow velocity of east asia

东亚地幔流动速度研究

effects of mantle flow on generation and distribution of global lithospheric stress field

地幔对流对全球岩石圈应力产生与分布的作用

Deep mantle flow, global tectonic pattern and the background of seismic stress field in China

地幔深部运动，全球构造格局及中国地震应力场背景

Results show that the thermal effect of plate motion driven mantle flow and its contribution to the observed heat flow is greater than that due to internal density anomaly ( tomography based).

结果表明，与地幔内部密度异常产生的热效应相比，运动的板块及其激发的地幔流动在全球地表观测热流的产生和分布特征上起着更为重要的作用。

Because of its special physical and chemical properties, the continental lithosphere does not actively take part in the convective mantle overturn. However it influences the convective flow and vice versa.

由于其特殊的物理化学性质，大陆岩石圈通常不直接参与下方的地幔对流，但其与地幔对流格局有着重要的相互影响。

The percentage of heat flow from mantle is bigger than 80% in terrestrial heat flow, whereas the percentage of lower crustal heat flow is smaller than 20% in terrestrial heat flow.

海盆区地幔热流在地表实测大地热流中所占比例高于80%，地壳下部热流在地壳总热流中所占比例小于20%。

The inner core ( IC) rotation relative to the mantle and the fluid outer core ( OC) flow due to the rotation are studied in this paper.

本文的主要内容是研究固体内核相对地幔的转动及其引起的液体外核流动。

The Earth's crust mainly by cracking, soft flow of the mantle layer, the liquid outer core, the core solid four components, one to the earth this is not a solidified body.

地球主要由龟裂的地壳、软流层的地幔、液体的外核、固体的内核等四部分组成，这样一来地球就不是一个凝固体。

mantle heat flow and deep temperature of jiyang depression, shandong, north china

济阳坳陷地幔热流和深部温度

this paper introduces the concept of mantle heat flow and its calculation method;

本文介绍了地幔热流的概念及计算方法，建立了相山地区的地壳结构模型和岩石放射性热源分布模型；

Our result shows the nonuniform distribution of mantle heat flow in China.

结果显示,中国大陆地幔热流的空间分布不均匀.