地壳变形与地下流体之间既相互联系又相互影响。
The mutual relation and influence between the crustal deformation and the subsurface fluid are present obviously.
低序次断裂是地壳变形的直接产物，具有丰富的构造变形信息。
Subordinate fault is the direct production of crust deformation, It has rich information of structure deformation.
地震前，地壳变形引起地球密度重新分布，从而使地球重力场发生某些特征变化。
Before earthquake occurrence, the crustal deformation causes redistribution of the earth density, so there occur some characteristic changes in the earth gravity field.
低序次断裂是地壳变形的直接产物，具有丰富的构造变形信息，经过转换的低序次构造。
Subordinate fault is the direct production of crust deformation, It has rich information of structure deformation.
通过应用卫星重力测量仪器和追踪地震导致的地壳变形，地质学家能够准确的预测将要发生的地震会发生在什么地方(但不能测出什么时候发生)。
Geologists can accurately predict where (but not when) the next earthquake will happen by using satellite gravity measurements and tracing ground deformation caused by earthquakes.
贝维斯团队希望在原有的二十五台GPS测量站的基础上，新增五十个GPS测量站，以便更好的测量即将延续多年的地壳运动和变形。
Bevis' team hopes to add 50 more GPS stations to its current 25 to better measure the movement and deformation of the crust that will continue for years.
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.
对地壳的流变特性和变质变形研究是当前地球系统科学研究的一个重要切入点。
The research on lithosphere rheology and deformation and metamorphism is an important cut-in point of earth system science.
讨论了将相对运动和应变变化综合起来以更充分地描述地壳运动和变形的模型。
The model of crustal movement and deformation, which is depicted fully by comprehending the relative motion and strain variation, is discussed.
综合考虑多因素和多过程间的耦合与反馈作用，建立了地壳演化与变形的综合的非线性动力学模型。
A comprehensive nonlinear dynamic model for the evolution and deformation of the crust is established based on considering the coupling and feedback among many factors and processes.
由此而产生力的作用，使地壳岩层变形、断裂、错动，于是便发生地震。
The resulting in the role of the crustal deformation of rocks, broken, dislocation and then the earthquake.
伽师强震群的破裂断层面为北东向，与震源深度梯度变化带、地壳接触变形梯度变化带、等烈度线以及地震扩展方向吻合；
The rupture surface is to NNE, similar to gradient belt of focal depth, gradient belt of crustal deformation, isoseisms and extended direction of earthquakes.
岩石圈具有温度高、强度低和强烈流变分层等特征，且下地壳表现为韧性流动变形。
The lithosphere beneath this area is associated with high temperature, low strength and intensive rheological stratification, and the lower crust is characterized by ductile flow deformation.
对川滇地区重力场特征进行了研究，获得了研究区内地壳厚度分布及变形特征。
Moho depth distribution and crustal deformation pattern between different sub-blocks in Sichuan-Yunnan region are presented here based on the studies of the gravity field characteristics.
现代地壳应力值高，构造变形速度快，地震活动强度加剧，地热流异常明显。
Present crustal stress values are high, structural deformation rate is fast, intensity of earthquake has an obvious increasing trend, and terrestrial heat flow anomaly is very obvious.
地壳中岩石的变形模式受构造应力、流体压力和上覆岩层重力共同作用的影响。
Deformation pattern of rocks in earth's crust is effected by tectonic stress, fluid pressure and gravity of the overlying strata.
流体流动和在地壳岩石变形过程耦合，生产机械和流体输送方式发生了复杂性。
Fluid circulation and deformation processes in crustal rocks are coupled, producing significant complexity of mechanical and fluid transport behavior.
这些伸展构造很显然是扬子克拉通和华北克拉通在三叠纪碰撞时，大别山造山带前陆位置岩石圈弯曲导致地壳上部产生非弹性变形的结果。
Such structure in the collision foredeep of the Dabieshan Orogen was resulted in inelastic extensional deformation of the conver side of the flexed plate aroused by lithospheric flexure.
第一个是扩散变形的大陆地区其地壳块体绕垂直轴的旋转的问题。
One of them refers to the rotation about vertical axes of crustal blocks in continental areas of diffuse deformation.
利用GPS观测结果研究了中国大陆当前地壳运动的空间分布及其所揭示的大区域构造变形背景与趋势；
This paper analyzes spatial distribution of current crustal movement in Chinese mainland, and large areal tectonic deformation background and trend with the GPS data.
另一部分是差应力，固体中受外力作用普遍产生差应力，它引起地壳物质变形，产生各种构造形迹。
Differential stress is commonly produced when external forces act on a given solid body. It may cause deformation of crustal materials and generate various kinds of structural features.
本文讨论了地壳和上地幔中韧性剪切带及其中的变形岩石。
This paper deals with the ductile shear zones and their deformed rocks in the crust and upper mantle.
这些实验研究结果对于地壳中浅层次构造变形及表层构造软弱带成因研究肯有重要意义。
The results of this experiment are very important to the research of the gene-sis of weak zone of the surface structures and the shallow structural deformation in the crust.
变质构造岩是由变质变形作用形成的一种特殊类型岩石，形成于地壳不同构造层次上的韧性变形带中，具有明确的构造成因的含义。
Metamorphic tectonite is a special rock formed by deformation in ductile shear belts at different crustal levels, which has a clear meaning of structural origin.
这种深部构造信息也有可能通过地壳的动力变形和深部地球化学反应传递到地表。
The deep structural informations are also probably transmitted through mechanical deformations and deep geochemical reactions to the earth's surface.
上地壳表现为脆性变形，中、下地壳为韧性的流动变形。
The middle crust and the lower crust is in the ductile field.
青藏高原新生代伸展地堑构造是高原经历早期地壳强烈缩短变形之后，在深部动力学机制作用下快速隆升的产物。
The Cenozoic extensional grabens on the Qinghai-Tibet plateau are the product of rapid uplift of the plateau caused by the deep dynamic mechanism after earlier strong crustal shortening.
地壳伸展变形强度弱，总体具有纯剪变形的构造几何特征，形成裂谷型盆地。
This structural style displays low-magnitude extension, has overall tectonic geometry of pure shear and forms rift basins.
由于岩石的塑性变形、弱化和强度的减小，以及从岩石中脱出的水的参与，这个带就成了地壳中的薄弱层和低速层。
Due to the plastic deformation, weakening and strength decline of rocks, and participation of water released from rocks, this zone becomes a weak interlayer in the crust and crustal low veloci...
断裂带在地壳浅部亦会发生部分韧性变形。
The shallow parts of a fault zone can also develop loeal ductility deformation.
应用推荐