It seems possible that a sinking current of cooled mantle material on the upper side of the plate might be the cause of such deep basins.
看来，板块上侧冷却的地幔物质的下沉流可能是造成这种深盆地的原因。
As the plates separate, hot molten mantle material flows up to fill the void.
随着板块的分开，炽热的熔融地幔物质向上流动，以填充空隙。
Upper mantle uplift is likely associated with upward migration of mantle material.
地幔上隆可能意味着地幔物质向上运移。
The previous researches indicate input of mantle material into upper crust during magmatism and ore-forming process.
大量研究资料表明，区内成矿和成岩过程中有幔源物质的加入。
It is a mixture of crust and mantle materials which resulted from the upwelling and transporting of the upper mantle material.
在下地壳下部有一数公里厚的高速致密的壳-幔混合物层，其形成原因是由于上地幔物质上涌并迁移到下地壳的结果。
The partial melting is caused by the heat derived from subduction and crust shortening rather than by the mantle material intrusion.
壳内局部熔融则来源于板块俯冲、地壳增厚产生的热而非幔源侵入所造成。
The theory is concerned with the vertical movement of deep-seated mantle material thus significant to the deep dynamic mechanism of the earth.
地幔柱理论涉及地幔深部物质垂直运动的机制，对了解地球深部动力学机制有重大意义。
Mantle material can sink at a plate boundary, and then flow back upward farther away, pushing on the crust - a process called small scale convection.
地幔，这种物质可以在板块边界处下沉，然后向上回流到较远的地方，再与地壳相碰撞——这个过程被称为小规模的对流。
It is revealed that the source of different types of metallogenetic granitic assemblages is mainly crustal materials, with mantle material adding.
揭示了不同岩石组合谱系类型成矿花岗岩类的岩浆源岩主要是地壳物质，具有地幔和地壳双重物源的特征。
The researchers discovered the "spin transition zone" by subjecting laboratory samples of lower-mantle material to high temperatures and pressures.
研究员通过服从低披风材料实验室样品发现了“旋转转折区域”到高温和压力。
The "mantle plume" thus formed, once established, continues to channel hot material from the mantle base until the reservoir is emptied.
这样形成的“地幔柱”一旦形成，就会继续从地幔底部引导热物质，直到储层被排空。
The mantle's motions, analogous to those in a pot of boiling water, cool the mantle by carrying hot material to the surface and returning cooler material to the depths.
地幔的运动类似于一壶沸水的运动，它把热的物质带到表面，再把较冷的物质带到深处，从而使地幔冷却。
In a titanic collision model, the bulk of the Moon would have formed from a combination of material from the impactor and Earth's mantle.
在泰坦尼克碰撞模型中，月球的大部分是由来自撞击者和地幔的物质结合形成的。
The implication is that the gases in the mantle came not from the sun but from the early accretion of rocky material.
这意味着地幔中的气体不是来自太阳，而是来自岩石物质的早期积累。
And another, even more important industrial material, petroleum, may also come from the mantle.
另外一种更加重要大的工业材料，石油，同样是来自地幔。
Underplating of basic melt beneath the crust is one of the most important patterns of crust growth and represents an effective material and energy transfer from the mantle to the crust.
基性熔体的下垫作用是地壳生长的一种重要方式，并且代表了一种有效的幔向壳的物质与能量迁移。
And another, even more important industrial material, petroleum, may also come from the mantle.
另外一种更重要的工业原料石油也是来自地幔。
The formation of these basins is directly connected with the motion of the Pacific and Eurasian plates and is restricted by the movement of the material in the deep mantle.
它们的形成与太平洋板块和欧亚板块的运动密切相关，并且受着深部地幔物质运移的制约。
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。
Then it is proposed that hydrogen is primary hot material in the mantle plumes.
从而提出，氢是地幔羽中的原始热物质。
Studies on geology, isotopes and metallogenesis indicate that the ore forming material derived from strata and magma derived from crust mantle.
对其矿床地质特征、同位素地质学、矿床成因等方面研究，认为成矿物质来源具双重性，既有来源于地层，又有来自壳幔源岩浆。
They were formed by mixing of the partial melting granitic magma of crust-derived material and mantle-derived basic magma.
岩石主要由幔源岩浆与中下地壳物质部分熔融形成的花岗质岩浆的混合形成的。
Projecting the lead isotope compositions on the Pb tectonic evolution model, the result indicates that the raw material of Jianchaling ultrabasic rock coming from the deplete upper mantle.
岩石铅同位素构造演化模式判别结果表明，煎茶岭超基性岩石的成岩物质来自亏损上地幔；
The metallogenic source material comes from the upper mantle and the lower crust.
成矿物质来源于上地幔和下地壳。
Material basement and migration dynamic are two essential problems that have to be answered by the crust mantle hydrocarbon abiogenesis theory.
油气生成的物质基础和运移动力是油气壳-幔非生物成因说必须回答的二个基本问题。
It is then presumed that the upper -mantle beneath the Qaidam Basin is rigid, where there is no exchange of hot material.
推测柴达木盆地的上地幔中没有热物质的交流，为刚性岩石圈。
It is then presumed that the upper-mantle beneath the Qaidam Basin is rigid, where there is no exchange in hot material.
推测柴达木盆地的上地幔中没有热物质的交流，为刚性岩石圈。
The ore-forming material and fluid was derived from the depth of the Earth especially from upper mantle or crust-mantle mixing zone , due to alkali-rich magma activity during late Yanshanian epoch.
成矿流体和主要矿质均源于地球深部，以上地幔或壳幔混合带为主，与燕山晚期富碱岩浆活动密切相关。
The ore-forming material and fluid was derived from the depth of the Earth especially from upper mantle or crust-mantle mixing zone , due to alkali-rich magma activity during late Yanshanian epoch.
成矿流体和主要矿质均源于地球深部，以上地幔或壳幔混合带为主，与燕山晚期富碱岩浆活动密切相关。
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