地震通常都伴随着火山活动或地球深处的岩浆运动。
Earthquakes commonly accompany volcanic activity on movement of magma deep in the earth.
是喜山运动早、中、晚三个岩浆旋迥的产物；
They were the products of the early-, middle- and late- magmatic cycles of Himalayan movement.
岩浆会朝着阻力最小的方向运动，也就是向北，因此会冲向现在加勒比或是中美洲的所有火山下方。
It will move in the direction of least resistance, which will be toward the north, and thus it will rush under all volcanoes currently in the Caribbean or in Central America.
流体运动和岩浆活动，对鸟取地震的成核和破裂过程有重大的影响。
The fluid transportation and magmatic activity have great influence to the nucleation and rupture process of the Tottori earthquake.
板块构造学说揭示了海底扩张和板块的水平运动现象，阐明了与板块边界相联系的岩浆活动。
The plate tectonic theory reveals the seafloor spreading and plate lateral movement, and illustrates magmatism related to plate boundaries.
区域经历了多阶段的强烈构造运动，而几乎每一次重要的地壳构造运动，都有相应的岩浆岩形成，具有多旋回岩浆活动特征。
Areas of experience and strong tectonic movement and almost every important crust tectonic movement, have corresponding magmatite, polycyclic magma activity.
原生裂缝是岩浆冷凝结晶过程中形成的裂缝；次生裂缝是火山岩及其原生裂缝系统受后期构造运动、溶蚀、风化等作用改造而形成的裂缝。
Primary fracture were formed during the lava crystal and the secondary fracture generated during the volcanic reconstruction by tectonic movement, and wind action, solution.
晶体分布参数S介于10 -7 ~ 10 -3间，显示岩浆中晶体基本上是自由浮动的，晶体的运动受流体的运动控制。
The crystals distribution parameter s values range from 10 ~ (-3) to 10 ~ (-7), indicating that the crystals were floating in magma and controlled by the movement of liquid.
豆荚状铬铁矿以其独特而稳定的物理化学特性，记录了大洋地幔深部岩浆活动(特别是扩张中心原始岩浆活动)以及大洋岩石圈运动过程。
As podiform chromitite has stable physical and chemical properties, it has recorded the magmatic process of the mantle under the ocean spreading centre and the lateral movement of oceanic lithosphere.
成矿机理是：区域板块运动使本区在侏罗纪末下地壳形成花岗岩浆熔融层。
The metallogenic mechanism is as follows: in the latest Jurassic, the melting layers of granite magma in the lower crust were formed by the regional plate movement.
构造运动往往伴随有岩浆活动，含矿流体在构造动力和岩浆热力的驱动下产生活化转移。
Tectonic movement sometimes go with magma activity, and make fluid which include ore elements occur activation and transfer with the tectonic dynamic and magma heat.
这两者之间的相互作用导致了流体外核的形成、玄武岩浆的产生、洋壳的形成、以及内核和地幔之间的差异旋转运动。
The interplay between the two leads to the formations of fluid outer core, basalt magmas, oceanic crust, and differential rotation between the inner core and mantle.
队伍认为一股滚热的固态岩浆从冰岛下面的一个热区升上来并且在地壳下面向东运动。
The team suggests that a pulse of hot, solid rock rose from a hotspot beneath Iceland and travelled east beneath the Earth's crust.
队伍认为一股滚热的固态岩浆从冰岛下面的一个热区升上来并且在地壳下面向东运动。
The team suggests that a pulse of hot, solid rock rose from a hotspot beneath Iceland and travelled east beneath the Earth's crust.
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