地核

Miles below the Earth's surface, there is a vast ocean of molten iron.

在地球表面2000英里之下，那儿有一个巨大的热火炉，这就是地核。

It means that dilapidated atoms pressed by self attraction produce differentiation according to the size of atomic density.

残破的原子在自引力作用形成的压力作用下，按原子密度的大小产生分异，"内核"多为显示有正电性能的密度较高的残破原子组成，"外核"为富含"公有化"电子而显示负电性能的密度相对较低的残破原子组成，这是一个地核物质量子状态变化的静态过程。

Because the core current is somewhat symmetrical around the axis of rotation, the associated magnetic field is similar to that of a bar magnet.

因为地核流在旋转轴周围存在着一些对称，所以相关的磁场与棒磁铁的磁场相似。

In this case,the source of the earth's magnetic field is the current produced by displacement of a double electrical layer's plates appearing on the boundary of the solid and liquid phases of the nucleus (the layer F of Bullen's earth's model).

在这种场合下，地球磁场的本源就是电流，这种电流是由在地核固相与液相边界上的一对带电层的相对运动产生出来的(Bullen地球模型中的F层)。

Earth's collision with another large celestial body after much of the Earth's iron fell to its core.

其他的理论家提出，在地球的大部分铁沉入到地核之后，由于地球与另一个庞大的天体发生碰撞，月亮便从地球那石质的地幔中撕裂开来而形成的。

In the around three-hour-movie hour, superheating centrosphere threatens human being.

在这部近3个小时的影片中，地核过热威胁人类。

We do not know much yet about the moon's mantle, that section of superheated rock which goes down hundreds of miles below the curst.

我们对月球地幔所知不多，那些过热的岩石在外壳几百英里以下。我们预料，但是我们不能确定，月球有一个由熔岩构成的地核，如同地球。

It seems likely that electric currents in the core of the earth are responsible for the observe geomagnetic field.

似乎很可能是地核内的电流引起了我们观察到的地磁场。

An upwelling of molten material from the earth's mantle .

地球的中心是地核，地核的周围是地幔。

A nucleoside, C10H14N2O5, composed of thymine and deoxyribose.

地球的中心是地核，地核的周围是地幔

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。