基本解释：地壳断裂
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Tycho Brahe: An important Danish astronomer of the 16th century. His ground breaking research allowed Sir Isaac Newton to come up with the theory of gravity.16世纪一个重要的丹麦天文学家。他的地壳断裂研究让牛顿得以提出重力学理论。
Faults are like cracks all over a teapot.地壳断层就像遍布茶壶表面的裂痕。
Faults are like cracks all over a teapot, except that they're moving all the time.地壳断层就像遍布茶壶表面的裂痕，只是这些裂痕会不断移动。
The fault is of brittle type in the shallow tectonic level of the earth's crust. The main deformational mechanism is cataclasis.该断裂为地壳浅部构造层次的脆性断裂,主要的变形机制是碎裂作用。
An earthquake is a shaking of the ground caused by the sudden breaking and shifting of large sections of the earth's rocky outer shell.地震是地球岩石外壳大范围的突然断裂和滑移所引起的地面摇动。
When this break occurs,or when the sides of an old break slip,the earth quakes,or shakes,while the crust is settling into a new position.当断裂发生时，或者旧的断裂块滑动时，地球震动、摇动，以使地壳安排它进入一个新位置。
WENCHUAN EARTHQUAKE M_S 8.0:PRELIMINARY STUDY OF CRUSTAL ANISOTROPY ON BOTH SIDES OF THE LONGMENSHAN FAULTS汶川M_S 8.0地震:龙门山断裂两侧地壳各向异性的初步研究
Forces in the earth's crust have been active throughout geological time. Rocks respond to these forces by folding and faulting.在整个地质历史时期，力始终作用于地壳之中，地壳岩石对这些力的反应就是褶皱和断裂。
The upwelling of the mantal substance along fractured zones may be the reason causing the abnormal crust and mantal structure.地幔物质沿断裂带上涌，可能是形成异常壳幔结构的原因。
Based on this, the relation between fracture fractal dimension and the Earth crust activity was discussed.在此基础上,讨论了断裂尺度分形维数与地壳活动性的关系。
Most of the faults in the southeast coast of Fujian Province occur in the sial of upper crust and some have reached the sima.福建东南沿海断裂1 多发生于上地壳硅铝层 ,少数达硅镁层。
FAULTING CHARACTERISTICS OF WENCHUAN EARTHQUAKE AND EVALUATION THEORY OF REGIONAL CRUSTAL STABILITY FOR ENGI NEERING龙山门断裂带活动特征与工程区域地壳稳定性评价理论
The Earth crust activity of different geotectonic elements could be estimated with the fracture fractal dimension.利用断裂尺度分布的分形维数值的大小,可以定性判断不同大地构造单元的地壳稳定性。
volcanic rift zone【地质】火山断裂带
An Analysis and Improvement of Rear Axle Case Fracture in N300 VehicleN300型客车后桥壳断裂的分析和改进
So the crustal stability of NorthwestYunnan is determined dominatingly by the active fault and seism.因此发现该区地壳稳定性主要受活动断裂和地震这两类因素的控制。
The process of mountain formation, especially by a folding and faulting of the earth's crust.造山运用，造山作用山脉的形成过程，特别是由于地壳的重叠和断裂造成的
Because of the great weight pressing down on them,these layers tend to fold downward at weak spots,and this finally causes an actual break in the crust.由于巨大重量向下压岩层，使它趋于在它的薄弱点处往下折叠，这最后将造成地壳里的某处断裂。
