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。
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。
The tectonic units of the continental lithosphere are mainly composed of the orogenic belt systems and associated basin systems.
大陆岩石圈的构造单元主要由造山带系统及其相关的盆地系统构成。
The formation and evolution of continental lithosphere has been one of important research projects in earth science field for these years.
绪论大陆岩石圈的形成与演化是近年来地球科学领域重要的前沿研究课题之一。
These studies indicate that the continental lithosphere is characterized by heterogeneities in its thermal state, chemical composition and mechanical behavior.
不同学科的最新研究成果表明，岩石圈在热状态、化学成分和力学行为等方面具有高度非均匀性。
Rupturing Continental Lithosphere, Subduction Factory, the Seismogenic Zone Experiment, and Source-to-Sink, for the field of ocean-continent margin researches.
该文献确定了洋陆边缘的4个主要研究领域，即大陆岩石圈裂解、俯冲带物质转换、地震带实验、源汇系统。
The extension of the continental lithosphere that gives rise to extensional basins is generally considered as a shear process on major, gently dipping normal fault.
形成拉伸盆地的大陆岩石圈伸展构造作用，一般认为是沿大型缓倾角正断层（滑脱断层）的剪切作用过程。
The rudimental guide of the plate-tectonic theory landing on continent is the archipelagic arc-basin system between the oceanic lithosphere and continental lithosphere.
大洋岩石圈与大陆岩石圈之间的多岛弧盆系构造域是板块构造登陆的入门向导。
In this model the EastAsia continent is limited in a trapezoid geological frame and the continental lithosphere is regard as a continuum thin plate with a power law rheology.
模型将东亚大陆限定在一梯形边界框架之中，大陆岩石层被视为由幂指数律控制的薄层，它上伏在粘滞性较低的软流层之上蠕变流动。
This theory could not explain the composition, structure and evolution of continental lithosphere and continental orogenic belt, and also is not in line with modern scientific theory.
上述理论阐明不了大陆岩石圈、大陆造山带的组成，结构与演化，也与当代的基础理论不尽吻合。
Therefore, it suggests vertical accretion of lithosphere in deep crustal setting of orogenic belts and shows its importance in continental dynamics.
该穹隆突出而重要地参与了秦岭造山带的形成与演化，具有重要的大陆动力学意义。
The author thinks that the ocean lithosphere delamination (OLD) is different from the continental lower crustal delamination (CLCD) in the paper: (1) the different delamination material.
本文认为，大洋岩石圈拆沉和大陆下地壳拆沉是不一样的：(1)拆沉的物质不同。
Netlike plastic flow in the lower lithosphere, as viscoplastic flow involving plastic flow network, controls tectonic deformation and dynamic processes within the continental plate.
岩石圈下层的网状塑性流动，作为包含塑性流动网络的黏塑性流动，控制着大陆板块内部的构造变形和动力学过程。
The main features of continental rift are mantle upwelling, extension, thinning, faulting and subsidence of lithosphere. The extensional environment is necessary and key to form a continental rift.
大陆裂谷以地幔上隆、岩石圈伸展、减薄、断陷和沉降为特征，伸展构造环境是大陆裂谷形成的必要条件和本质特征。
Panxi Rift with the dome-shaped volcano pattern has undergone three evolutionary processes: the lithosphere dome by mantle bulge, the continental crust dome and the subvolcano-dome.
本文主要讨论穹窿-火山型攀西裂谷的成因，岩浆深成作用与火山作用过程；
Panxi Rift with the dome-shaped volcano pattern has undergone three evolutionary processes: the lithosphere dome by mantle bulge, the continental crust dome and the subvolcano-dome.
本文主要讨论穹窿-火山型攀西裂谷的成因，岩浆深成作用与火山作用过程；
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