本文对近年来大陆岩石圈流变学的研究进展进行了综述。
Here we summarize the advancement in studying on rheology of continental lithosphere in recent years.
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 tectonic units of the continental lithosphere are mainly composed of the orogenic belt systems and associated basin systems.
大陆岩石圈地幔的古老形成年龄与上覆地壳克拉通的古老稳定年龄相耦合。
The ancient formation age of continental lithospheric mantle is coupling with the age of overlying craton crust.
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。
Particularly, for the continent, the crust thickness, thermal age and strain rate significantly had strong effect on the lithosphere strength.
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。
The rudimental guide of the plate-tectonic theory landing on continent is the archipelagic arc-basin system between the oceanic lithosphere and continental lithosphere.
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。
The formation and evolution of continental lithosphere has been one of important research projects in earth science field for these years.
基于大陆根柱构造概念，讨论了新生代以来中国大陆岩石圈尺度的大地构造分区。
Based on the concept of continental roots plume tectonics, geotectonic units of China continent on a lithospheric scale since Cenozoic are discussed in this paper.
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。
Responses of continental lithosphere to structuring, gravitation and thermodynamics largely depend on its rheological strength.
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。
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.
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 extension of the continental lithosphere that gives rise to extensional basins is generally considered as a shear process on major, gently dipping normal fault.
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 effective elastic thickness of continent can correspond to only a part of the lithosphere, not to the total lithosphere.
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。
Rupturing Continental Lithosphere, Subduction Factory, the Seismogenic Zone Experiment, and Source-to-Sink, for the field of ocean-continent margin researches.
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。
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.
海洋板块是由密度更大、更重的岩石构成的，所以它开始下沉到大陆板块之下，到地幔之中。
The oceanic plate is made of denser and heavier rock, so it begins to sink down under the continental plate and into the mantle.
海洋板块的岩石，玄武岩，以及覆盖其表面的沉积物被拉沉到海洋底部，充当移动大陆的传送带机制的一部分。
The ocean floor rock, basalt, along with the sediment that built up on top of it, was drawn down at the edge of an ocean as part of the conveyor-belt mechanism that moves the continents.
今天，约3000名修道士生活在散布于大陆或高处于岩石岛屿上的200所修道院中。
Today, about 3,000 monks live in the 200 stand - ing monasteries scattered around the mainland or perched on rocky island sites.
如今构成加拿大北极群岛的岩石在数百万年以前只是一个叫Pangaea(泛古陆)的超大陆西北海岸以外的海底沉淀物。
Rocks that now make up the northernmost islands of the Canadian Arctic formed millions of years ago as seafloor sediments off the northwestern coast of a supercontinent called Pangaea.
为了研究，Loewy和同事们收集了北美中大陆断裂系中一块区域的岩石。
For their study, Loewy and colleagues collected rocks from a region known as the North American Mid-continental Rift System.
在崎岖多石的地形下面，埋藏着岩石和化石，这有趣地说明远古时代的大陆板块碰撞，形成了现在的地貌、气候和植被。
The rocks and fossils buried in this rugged landscape tell an intriguing story of an ancient collision that shaped the modern topography, climate, and plant life.
龙虾生活在大陆架边缘海岸处的岩石，沙土，或泥底。
Lobsters live on rocky, sandy, or muddy bottoms from the shoreline to beyond the edge of the continental shelf.
这次撞击将能够告诉我们答案的痕迹留在了岩石里——包括岩石中一个1英寸（约2.54厘米）厚的黑色煤灰层，之前这个煤灰层一直被认为是由地球大陆上广泛扩散的野火造成的。
The collision left behind tell tale traces in the rocks - including a black 'mat' of soot an inch thick thought to have been created by continental wide wildfires.
就像在北美大陆被压迫为弓形时发生的，当岩石碎裂时，地表水沿着新的路径流过裂缝。
When rock fractures, as is occurring in the N American continent while it is stressed into a bow, ground water follows new paths through the fractures.
对应每一旋回，喀喇昆仑地层区和塔里木地层区发育有被动大陆边缘盆地和碰撞造山两种类型的岩石组合。
For Kala Kunlun and Tarim, two kinds of rock associations, passive continental marginal basin and collision orogenic belt, are developed corresponding to each cycle.
铁锰结壳的铼-锇同位素组成明显有别于大陆地壳岩石，和K- T界线沉积物相似，接近陨石值。
The Re Os isotope composition is obviously different from the rocks of the continental crust, but similar to the K T boundary sediment, and close to the meteorite.
大陆的中心几乎与阿尔卑斯山等高，然而，超声探测显示，岩石底部的许多地点都低于海平面。
In the heart of the continent it is almost as high as the summits of the Alps, yet soundings show that in places that rock floor is below sea level.
蒙脱石除源于大陆派生的岩石风化物外，主要来自火山物质的蚀变。
Smectite mainly came from the alteration of volcanic ash or volcanic glass and the weathering materials derived from land rocks.
蒙脱石除源于大陆派生的岩石风化物外，主要来自火山物质的蚀变。
Smectite mainly came from the alteration of volcanic ash or volcanic glass and the weathering materials derived from land rocks.
应用推荐