相反,它们是其他类型的火山,比如地层火山,是板块运动的结果。
Instead, they are other volcano types, like strata volcanoes, for example, which are a result of the tectonic plate movement.
这些火山没有一个是由于火星地壳板块之间的碰撞而形成的——火星上没有板块运动。
None of these volcanoes was formed as a result of collisions between plates of the Martian crust—there is no plate motion on Mars.
地球内部因放射而产生的热量为板块运动、大陆漂移、造山运动和地震提供了能量。
Earth's internal heat, fueled by radioactivity, provides the energy for plate tectonics and continental drift, mountain building, and earthquakes.
板块运动是地幔运动的表面现象。地幔是位于地壳和金属内核之间的一层厚厚的岩石壳。
Plate movements are the surface expressions of motions in the mantle—the thick shell of rock that lies between Earth's crust and its metallic core.
初步探讨了板块运动的地球重力学机制。
Earth gravity mechanism for plate motion is investigated primarily.
板块运动是非常危险的。
板块运动是地壳和上地幔变形的主要动力来源之一。
Plate motion is one of the major dynamic sources for crustal and mantle deformation.
海底峡谷,是由于地壳板块运动而形成的一种地质构造。
Submarine canyon is a geological structure that formed by plate movement in the crust.
地球内部的热量在各个地方不均匀,由此导致了板块运动。
The heat within Earth is not the same everywhere and the plates move due to the heat.
至今还没有完整理论阐明板块运动的驱动力和地幔对流机制。
No comprehensive theory accounts satisfactorily for the driven force of plate motion and mechanism of mantle convection.
如果震中位于海底,板块运动带动上方海水起伏,形成波浪。
If the epicentre is on the seabed, that also lifts the water above the bed, creating a wave.
太古宙麻粒岩带就是太古亩地壳发生刚性板块运动的直接产物。
Archaean granulite belts are just the product of plate-tectonic movement of rigid Archaean crust.
地质学家把板块运动及这种运动所造成的后果看作是板块构造运动。
Geologists describe the motion of the plates and the consequences of such motion as plate tectonics.
这种情况发生时,一个板块运动到另一之上,突然导致地球表面断裂。
When this happens, one plate moves past the other, suddenly causing the Earth's surface to split.
GPS等测量显示的全球板块运动在一定条件下反映地幔顶部的水平流动。
Under certain conditions, the global plate motions revealed by GPS and other measurements reflect the horizontal flow in the uppermost mantle.
分析现代脉冲星的观测资料,有助于研究板块结构,板块运动和地震预报。
We may research into the plate structure, plate motion and earthquake forecast by analysing observed data of modern pulsars.
这与用其它资料分析的结果一致,可能的机制是岩石圈板块运动和地幔对流。
It is consistent with the results obtained from other data. The possible mechanism is lithosphere plate motion and mantle flow.
到目前为止,几乎全部有关板块运动驱动力源的研究,都把着眼点集中在地球内部。
Up to now, almost all researches of the driving force source of the plate movement concentrate the strarting point at the earth interior.
但是它确实坐落在在极移之前的板块运动期间和极移本身的时候注定要被拉下的区域。
But it does lie in the area destined to be pulled down during the plate movements preceding the pole shift and certainly during the pole shift itself.
分析了全球密度异常与板块构造的关系,探讨了全球密度异常分布对板块运动的作用。
The relation between global density anomalies and plate tectonics is discussed. And the action of density anomalies to plate moving is analyzed also.
板块构造的运动和动力学是地学研究的前沿课题。板块边缘强震是板块运动的直接结果。
The kinematics and dynamics of plate tectonics are the frontal subjects in geoscience, and the strong earthquake occurred along the plate boundary results directly from plate movement.
这些密封的金属盒子确实是外星人在重要海岸线沿途放置的防止板块运动的突然和颠簸的装置。
These sealed metal boxes are indeed alien, placed along significant coastlines to abort sudden and jolting plate movements.
在我们靠近更多的板块运动,更多的岩层压力,进入到极移的时刻之际,这是人类应该惊恐之事吗?
Is this a matter mankind should be alarmed about as we approach even more plate movement, more pressure on the rock stratas, going into the time of the pole shift?
事实上,这种冷却过程为地幔的缓慢流动提高了动力,驱使着板块运动,实现无止境地重塑地球表面。
It is in fact this cooling which powers the slow circulation of the mantle, and through that the endless remaking of the surface through plate tectonics.
从板块运动的观点出发,推断了半岛地壳的现代应力场、半岛地区的运动总趋势及其地震发生原因。
The current stress field of the crust, the general movement tendency and the causes of the quakes in the Penisula were inferred based on the plate tectonics.
该领域的其中一方面是要研究地震学---只有在板块运动剧烈的时候才会出现地震波并产生联动。
One segment of this field is devoted to seismology, the study of seismic waves that are generated when major geological shifts occur.
该领域的其中一方面是要研究地震学---只有在板块运动剧烈的时候才会出现地震波并产生联动。
One segment of this field is devoted to seismology, the study of seismic waves that are generated when major geological shifts occur.
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