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断层作用

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The earthquakes mainly show normal or strike-slip faults in Yajiang, North-triangle and west o f Chengdu-block areas, indicating that the vertical forces have been pl aying an important role in the source stress fields, while the earthquake mainly show reverse or strike-slip faults in Baoxing-Tianquan area, with the horizon tal compone nts of the principal pressure stress axis identical to the south-west directi on to which the shallow mass was moving.

雅江、 北三角和成都地块西部3个分区,地震破裂以正断层、走滑型为主,表明垂向作用力在震源应力场中发挥了不可忽视的作用宝兴天全地区的地震以逆断层、走滑型为主,其主压应力轴水平分量与浅层物质运移的南西方向一致。

3D-FEM computation model included 41 items of large structures and 5 items faultage s in the real attitude and distribution at the No.

根据结构面和断层的实际产状建立了包含41条长大结构面及5条断层的三峡大坝左厂3号坝段和4号坝段联合作用的三维有限元模型,模型中的结构面采用Goodman节理单元。

The paper has analysed the charactors of the mylonitic faultage in Yanmenguan Tunnel, especially in different structure stress field and different structure movement.

本文重点研究了发育在雁门关隧道左线糜棱岩构造破碎带的特征,分析了它形成、发展的规律,着重研究了该断层在不同构造应力场的作用下,所产生的不同期次、不同性质的构造运动的力学行为,并由此推断出该断层对隧道施工可能造成的影响,提出了行之有效的治理措

We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry.(1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin.(2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively.(3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt.(4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau.(5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure.

在综述前人认识的基础上,笔者通过对中国前陆盆地的构造演化历程、沉积充填特征、构造成因及其空间分布规律、构造变形特征等的研究,提出了中国前陆盆地构造地质发育的5个主要特征:(1)两种不同性质的原型盆地发生正反转的叠合性,即挤压构造下作为&本体&的前陆层序与拉张构造下作为&基础&的裂谷、断陷盆地之间的叠置;(2)显生宙以来中国大陆先后发生了4期前陆冲断构造演化的多期性,它们分别是加里东晚期、海西晚期、印支期和喜马拉雅晚期;(3)基于小克拉通基底拼贴后在造山带前缘复活再生的继承性,即统一拼合大陆内部的构造变形导致古造山带的复活,在古造山带边缘发育新生代前陆盆地或前陆冲断带;(4)在空间分布上受环青藏高原巨型盆山体系控制发生陆内变形的系统性,在环青藏高原巨型盆山体系内构造变形强度、盆地沉降幅度、盆山耦合程度等从内环向外环依次降低,从古造山带向克拉通方向构造变形强度依次降低,构造变形样式逐渐简单、构造变形时间依次变新;(5)前陆冲断带的构造样式由于受边界力学条件和沉积地层介质作用而具有多变性,存在沉积盖层内脆性变形的断层相关褶皱、造山带前缘韧性变形的基底卷入构造、与走滑构造相伴生的基底卷入的断层相关褶皱、盆地内部塑性变形的盐构造。

The four structural belts with different directions are found in the area. The faults with NE, NEE and NS trends formed earlier with long-term activity, and control on the basin evolution; the faults with NW trend formed later and overprinted on the early structures.

研究区主要发育4个方向的构造带,其中北东向、北东东向和南北向断层带形成较早且长期活动,控制了盆地的形成;北西向断层带形成较晚,对上述3个方向构造主要起改造作用。

In order to perfect the theoretical system of "tectonic control of hazard", this thesis researches the control function of stratum inclination of monoclinic structure, fold shape and angle between two limbs of fold, normal fault direction of dip and fault inclination, forms of faults combination over coal-mining-induced subsidence by means of theoretical analysis and numerical testing.

为了进一步完善&构造控灾&理论体系,本文从典型煤矿区的地质条件和开采实际出发,在以往研究成果的基础上,通过理论分析和计算机数值试验,重点研究单斜构造的地层倾角、褶皱构造形态及其翼间角、正断层倾向和倾角及断层组合对采煤沉陷的控制作用。

The east part is formed by overlapping of rollover anticlines generated by listric Chennan fault and sub listric faults in its hanging wall.

东段是由犁式陈南断层形成的大型滚动背斜和其上盘的次级犁式断层形成的滚动背斜叠加而成;西段是盐拱作用形成的底劈构造。

In this paper, by using of a COCT system, articular cartilages with an animal model are studied. Layer structures formed on the COCT images are investigated in theory and experiments.

本文用传统光学相干断层成像系统以动物模型对关节软骨进行了研究,对软骨组织的传统光学相干断层图像的层结构随脱水和机械作用的变化进行了分析。

According to the underground pressure theory, which takes stratum movement as key matter, the reactivating mechanical mechanism of a fault in mining floor under the action of underground pressure, and the mechanism of the interaction between pressure water and rock during the fault reactivation are studied.

根据&以岩层运动为中心&的矿山压力控制理论,研究了采场断层在矿山压力作用下活化的力学机制,以及断层活化过程中承压水和岩石相互作用的机理。

According to the underground pressure theory which takes stratum movement as key matter, the reactivating mechanical mechanism of a fault in mining floor under the action of underground pressure, and the mechanism of the interaction between pressure water and rock during the fault reactivation are studied.

基于大量的煤矿井突水案例,总结了中国煤矿井突水的一般规律及肥城煤田矿井突水的特点。根据&以岩层运动为中心&的矿山压力控制理论,研究了采场断层在矿山压力作用下活化的力学机制,以及断层活化过程中承压水和岩石相互作用的机理。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。