岩石构造的稳定性：第5届不连续变形分析国际会议录。
Stability of rock structures: proceedings of the 5th International Conference on Analysis of Discontinuous Deformation.
除了图中绿色的部分，这些气候严寒，主要为岩石构造的岛屿上，只有极少数低矮植物可以生存。
Despite the green hues in this image, these rocky islands are too cold to sustain more than a smattering of low-growing vegetation.
黏土和砂岩都是不坚固的岩石构造。
解释可能是在地球的地幔中，这是在构造板块下面的岩石层，向下延伸超过1800英里到地球铁芯的外边缘。
The explanation may be in Earth's mantle, the layer of rock underlying the tectonic plates and extending down over 1,800 miles to the outer edge of Earth's iron core.
地球表面并不是由构成地壳的单块岩石构成，而是许多紧密相连的“构造板块”，像一块巨大的拼图。
Earth's surface is not made up of a single sheet of rock that forms a crust but rather a number of "tectonic plates" that fit closely, like the pieces of a giant jigsaw puzzle.
在会聚的地壳或压转岩石中发生的走滑断层以正花构造向上断裂。
Strike-slip faults occurring in the converging crust, or transpression, rocks are faulted upward in a positive flower structure.
所以这将成为可能，就是，增强的构造活动和气候的变化腐蚀了含磷丰富的岩石，并在一个数百万年的时间内冲入大海。
So it's possible that enhanced tectonic activity and a change in climate eroded large amounts of phosphorous-rich rocks, which washed into the ocean over a period of several hundred million years.
这些岩石不像黄山的巨石，而是呈现出树干的构造，形状各异。
These rocks are not the giants of Huangshan, but more tree trunk-like formations of various shapes.
这个区域标志来自火山柱主要边缘的热度正在把岩石往上拱，如构造作用力导致火山柱向东方漂移。
This region marks where heat rising from the leading edge of the plume is pushing rock up, as tectonic forces cause the plume to drift eastward.
在一些走滑断层产生于聚敛地壳内或处于转换挤压作用下的地区内，岩石向上断裂成一种正向花状构造。
In areas where strike-slip faults occur in converging crust, or transpression, rocks are faulted upward in a positive flower structure.
典型的运移作用出现在由构造低的地区到构造高的地区，因为和周围岩石相比，烃类有相对的浮力。
Migration typically occurs from a structurally low area to a higher area because of the relative buoyancy of hydrocarbons in comparison to the surrounding rock.
他对鸟的飞行和水的流动、岩石的构造等都做了引人注目的阐述。
He made remarkable observations on the flight of birds, the flow of water, the structure of rocks.
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。
Tectonic fluids are concerned with those produced and participating in the tectonic event at all depths of 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。
The rudimental guide of the plate-tectonic theory landing on continent is the archipelagic arc-basin system between the oceanic lithosphere and continental lithosphere.
帕米尔地区碰撞构造的岩石与同位素年龄，记录了印度板块对亚洲板块的运动，经历了俯冲、碰撞和榨挤3个阶段。
The rocks and isotopic age of collisional structures in Pamir Plateau recorded the movement of Indian plate towards Asian plate, which passed through 3 stages of subduction, collision and squeezing.
岩石磁组构反映的应力状态总体为以NE向挤压为主，与轴向NW的背斜构造发育相一致。
The stress state reflected by the rock magnetic fabric is mainly manifested by NE compression, which is consistent with the arrangement of the anticlines with axes running NW.
然后从沉积微相分析入手，研究了沉积相标志，包括地层岩石的颜色、沉积构造、粒度分布、古生物学等。
Then, beginning with the microfacies, signs of sediment facies, including rock's colour, sediment structure, granularity distribution, fossil and so on, are studied.
构造裂缝的发育受岩石本身的力学性质以及局部构造制约，区域裂缝则与区域应力场强度有关。
The growth of structural fracture is controlled by such factors as lithology, porosity, lamellation and local structures, and the regional fracture controlled mainly by the regional stress field.
处在挤压变形带、剪切变形带到引张变形带(及地域)中岩石所承受的构造附加静水压力有逐次变小的规律性。
There is a gradual decrease in tectonic superimposed hydrostatic pressure from compressional deformation zone through shear deformation zone to extensional deformation zone.
复杂的地质构造，齐全的地层岩石，强烈的新构造运动控制着天然矿泉水的形成条件。
The formation of the natural mineral water controlled by the complex geologic structure, complete strata and rock, and strong neotectonism.
由岩石的构造破裂作用所产生的一种次生孔隙的类型。
A type of secondary porosity produced by the tectonic fracturing of rock.
湖南雪峰弧形构造带中的苗儿山韧性剪切带存在糜棱岩和片理化岩石两大构造岩类，各具不同的变形特征。
In Xuefeng arcuate structural belt of Hunan, Miaoershan ductile shear zone includes two types of tectonites, mylonite and schistosity rocks, which have different deformed characteristics.
板块构造学主要在于探索岩石田块体的运动，属于动力大地构造学范畴。
Plate tectonics explores primarily the motion of lithospheric blocks and belongs to the category of dynamic geotectonics.
拥有丰富的复杂地层条件下项目设计和施工的岩土工程经验，例如围垦、软土、多块石的基层、岩石构造等。
He has extensive geotechnical experience both in the design and construction for projects in challenging ground conditions i. e. reclamation, soft ground, bouldary bed, rock formation etc.
鉴别岩石的结构构造。
构造不仅可成为容矿构造，而且还控制蚀变岩石的分布。
The structure can become the host structure and control the distribution of altered rocks.
后重新研究了岩石的结构和构造及地下水的渗透方式，分析了紊流理论的应用界限。
Then the texture, structure of rock and seepage manner of groundwater were studied further. The application ranges of turbulent theory were also analyzed.
后重新研究了岩石的结构和构造及地下水的渗透方式，分析了紊流理论的应用界限。
Then the texture, structure of rock and seepage manner of groundwater were studied further. The application ranges of turbulent theory were also analyzed.
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