These dissolved materials thus pass from the lithosphere to the hydrosphere.
因此，这些溶解了的物质就从岩石圈转移到水圈。
As the plates spread apart, the lithosphere, or crust, is moved aside like a lid, allowing molten rock from the liquid asthenosphere to seep through.
板块分离时，岩石圈或地壳象盖子般移到一旁，液态软流层中的熔岩渗溢而出。
The global environment consists of the atmosphere, the hydrosphere and the lithosphere in which the life-sustaining resources of the earth are contained.
全球环境由大气圈、水圈和岩石圈所组成，其中包含了维系地球上生命的资源。
Scientists call this layer of crust and upper mantle the lithosphere.
科学家称这层地壳和上部地幔为岩石圈。
Variation of intrinsic energy of the lithosphere results in forming and perishing of rocks.
岩石圈内能变化导致岩石的形成和消亡。
Meanwhile, the fluid pathway in the lithosphere is also an important matter in volcanic researches.
同时，岩石圈内的流体通道也是火山研究中必须面对的一个重要问题。
The shear belt is one of the major structures widely developed in the earth's crust and the lithosphere .
剪切带是地壳和岩石圈中广泛发育的主要构造类型之一。
The effective elastic thickness of continent can correspond to only a part of the lithosphere, not to the total lithosphere.
大陆岩石圈等效弹性厚度往往只与岩石圈内部的某些岩层相关，因此它可能不代表一般意义上的岩石圈厚度。
The fluctuation of hydrograph in deep wells records the fluid pulsation in the lithosphere and variation of the Earth's crust.
深部含水系统水文过程线的波动在很大程度上记录了岩石圈的流脉动及一些地质过程的定向变化。
The existence of embedded high velocity thin layers in lower lithosphere may be of significance in the evolution of the lithosphere.
岩石圈中薄层的存在对于岩石圈的演化过程具有重要的意义。
Particularly, for the continent, the crust thickness, thermal age and strain rate significantly had strong effect on the lithosphere strength.
尤其对于大陆岩石圈，地壳厚度、年龄和应变率均可显著影响岩石圈的强度。
The characters of the lithosphere structure is studied by using the data of the MT in the transition zone between Jiamusi massif and Xingkai massif.
利用MT资料研究位于佳木斯地块和兴凯地块之间过渡地带的岩石圈结构特征。
Such variations in properties further indicate the complexity of the formation processes and evolution of the lithosphere over long geological periods.
性质和结构的差异体现了岩石圈形成和长期演化过程的复杂性。
Using general finite element program ANSYS, we simulate a dynamical evolution process of the lithosphere of west Liaoning, northeast China in the late Mesozoic.
利用大型通用有限元分析软件ANSYS简单模拟辽西地区中生代末期岩石圈动力学演化过程。
The study establishing the vertical structure of the lithosphere shows tectonic relationship of the western Qinling orogenic belt and Zoige Basin at lithosphere scale.
本次研究建立的岩石圈垂向构造图也展现了西秦岭造山带与若尔盖盆地的岩石圈尺度构造关系。
The lithospheric structure is to certain extent in accord with the geotectonic unit, suggesting that the crustal structure is influenced and restricted by the lithosphere.
中国岩石圈结构在某种程度上与大地构造单元相吻合，说明地壳构造受到岩石圈的影响和制约。
The pressure gradient of the lithosphere is a key to explain various geological processes, and it changes complicatedly with time and space as the geothermal gradient does.
岩石圈中的地压梯度是一个极为重要的参数，直接影响着各种地质作用的解释。
In evolution history of he lithosphere, the relative strength and acting way of the above forces determine the characteristics and driving mechanism of the lithosphere movement.
在岩石圈演化历史上，上述不同性质力源的相对强弱和作用方式，决定了岩石圈运动的性质及其驱动机制。
Sedimentary basin forming dynamics system is the macroevolution and correlation of the sedimentary basin, the mantle, the asthenosphere, the lithosphere, and Moho discontinuity.
成盆动力学系统是一个包括沉积盆地及其下的地幔、软流圈、岩石圈和莫霍面等不同地质单元的宏观变化和相互制约的过程。
The rheology boundary within the mantle lithosphere, the nature of the lithosphere, the intraplate stress and thickness, the sedimentary loading are the important geodynamic f...
地球内部流变学界限、岩石圈的性质和厚度、板内应力和沉积负荷是盆地形成的地球动力学基本机制。
The inversion results indicate as follows: 1, the lithosphere density beneath Chinese Sea and Its Adjacent Regions is extremely inhomogeneous. It shows the feature of violent tectonic movement.
反演结果表明：（1）中国海及邻域岩石圈密度极不均匀，反映了区内强烈的构造活动特征；
The second paper concerns itself with lithosphere dynamics and its application, and in particular it reviews several methods and the"geological pressure gauges"for measuring stress in the lithosphere.
第二篇文章是关于岩石圈动力学的研究及应用，着重介绍了估算岩石圈应力的方法和几种估算岩石圈应力的“地质压力计”；
The lithosphere thickness and bottom temperature of this region have been derived by making use of the averaged heat flow of the four regions.
并用四个地区的平均热流值推导出该区的岩石圈厚度和底部温度。
The lithosphere is divided into a few dozen plates of various sizes and shapes, in general the plates are in motion with respect to one another.
岩石圈被划分为几十个大小不同形状各异的板块，一般而言这些板块都处于相对运动之中。
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.
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-asthenosphere interaction zone is also a major component of the magma source, which consists predominantly of asthenospheric mantle and in the main contains no crustal component.
岩石圈-软流圈的作用带也是重要的岩浆源区，源区是以软流圈地幔为主，基本不含地壳组分。
The lithosphere-asthenosphere interaction zone is also a major component of the magma source, which consists predominantly of asthenospheric mantle and in the main contains no crustal component.
岩石圈-软流圈的作用带也是重要的岩浆源区，源区是以软流圈地幔为主，基本不含地壳组分。
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