• Even the planet's outer skin, or lithosphere, has been transformed.

    甚至于地球的表层——岩石圈——也已经被改变了。

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  • 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。

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  • 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。

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  • 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。

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  • The earth is a multi-layered rotating system, which is mainly made up of aerosphere, hydrosphere, lithosphere, mantle, outer core and inner core.

    地球是一个多圈层的旋转系统,主要由大气圈、水圈、岩石圈、地幔、外核以及内核组成。

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  • 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。

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  • The hydrosphere and the lithosphere together form the Earth's surface.

    水圈与岩石圈一起形成地球的表面。

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  • The Earth's lithosphere is formed of a rather small number of major plates.

    地球的岩石圈是由少数大板块所组成的。

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  • The tectonic stress in the Earth are mainly concentrated on the upper lithosphere.

    地球内部构造应力主要集中于岩石圈上层。

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  • Earthquakes along benioff zones are distributed in the descending lithosphere slabs.

    贝尼奥夫带的地震都分布在下降岩石圈板块内。

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  • 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。

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  • Various structural elements in the crust and lithosphere are interrelated and interdependent.

    地壳岩石圈中的各种构造要素是相互关联和相互依存的。

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  • Extensional crustal detachment is the most important tectonic response of lithosphere thinning.

    伸展条件下的地壳拆离作用是岩石圈减薄的重要浅部构造响应。

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  • 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。

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  • Here we summarize the advancement in studying on rheology of continental lithosphere in recent years.

    本文对近年来大陆岩石圈流变学的研究进展进行了综述。

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  • 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。

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  • The orogenic types were controlled by the relative motion mechanism between lithosphere and asthenosphere.

    板块和软流圈之间不同的相对运动机制是形成不同类型造山作用的主要原因。

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  • The dynamic model of lithosphere thinning in Jiaodong area is set up on the base of comprehensive analysis.

    在综合分析基础上建立了胶东地区岩石圈减薄的动力学模式。

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  • Notice first that there could be a substantial difference between lithosphere thickness and plate thickness.

    首先要注意:岩石圈厚度和板块厚度之间可能有重要区别。

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  • Some times in the process there was reworking of diapir of mantle-sourced magma on the crust or lithosphere.

    在某些地质时期还与幔源岩浆的底垫对地壳或岩石圈的改造有关。

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  • Some advances of many scholars studying on lithosphere thinning in eastern China in recent years are reported.

    介绍了近年来不同学者从各个方面研究中国东部岩石圈减薄所取得的进展。

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  • Paleogeotherm is important for understanding the thermal structure of lithosphere at a specific geological time.

    古地温曲线是岩石圈在特定地质时期热结构的集中体现。

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  • Tectonic fluids are concerned with those produced and participating in the tectonic event at all depths of lithosphere.

    构造流体系指岩石圈不同层次构造活动中产生的流体以及积极参与构造作用的流体。

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  • The spatial variation of lithosphere rheological property produces structural weak zones where deformation easily happened.

    岩石圈流变性的空间变化产生了构造上的软弱带,成为极易变形区域。

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  • The research on lithosphere rheology and deformation and metamorphism is an important cut-in point of earth system science.

    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。

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  • 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。

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  • It is consistent with the results obtained from other data. The possible mechanism is lithosphere plate motion and mantle flow.

    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。

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  • Responses of continental lithosphere to structuring, gravitation and thermodynamics largely depend on its rheological strength.

    大陆岩石圈对构造作用、重力作用和热作用的响应在很大程度上取决于其流变强度。

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  • The hydrosphere, atmosphere, pedosphere, lithosphere, biosphere, and energy circle in an ecosystem are also in a dynamic balance.

    生态系统中的水圈、气圈、土石圈、生物圈、能量圈也呈动态平衡。

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  • The hydrosphere, atmosphere, pedosphere, lithosphere, biosphere, and energy circle in an ecosystem are also in a dynamic balance.

    生态系统中的水圈、气圈、土石圈、生物圈、能量圈也呈动态平衡。

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