- 更多网络例句与剪断层相关的网络例句 [注：此内容来源于网络，仅供参考]
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Based on systematic structural interpretation with 3D seismic data and analysis on regional geology and drilling data, the fault system and tectonic style of the Yitong Graben are studied.
通过对三维地震资料进行系统的构造解析，结合区域地质和钻井资料的分析表明，伊通地堑的断层系统在平面上主要由近东西向的张性正断层和北东走向的张剪性断层组成，反映盆地具右旋走滑的应力体制；断层在演化序列上分为4个类型，与盆地的形成和演化之间存在良好的对应关系。
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Dislocation and stress drop on the strike or normal fault were obtained. In the second stage of dynamic analysis, the time-dependent shear stress release was applied on the fault plane to excite fault movement and ground vibration.
然后以断层面上的剪应力释放作为外部动态荷载，进行了断层运动的动态分析，通过数值计算得到震源断层附近的地面加速度、速度与位移的时间过程。
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And the results indicate that the principal stress directions in study area are mainly NE-SW, and the second substage tectonic twist made the direction deflect from North to East, but the primary direction changed little; tectonic activities during the O〓～S～D stage is some violent, most of the area are under high stresses status, and rock fracture degree is correspondingly higher, as coinciding with the drill cores observation, i.
通过数值分析，模拟了塔中Ⅰ号断裂带和塔中45井三维模拟区O〓灰岩的构造应力场和应变场，结果表明：研究区主应力方向为北东～南西向，第二期的构造扭动使其由北向东发生了一定的偏转，但总的方位变化不大；O〓～S～D时期，塔中地区构造运动较强，研究区大部分处于高应力状态，岩石破裂程度较高，而岩芯观察结果也证实了这一结果，即O〓灰岩地层中早期形成的构造结构面比较发育，单个结构面的规模也较大；C～P时期，岩石的破坏程度较早期有所提高，主要表现在两个方面，一是各局部区岩石的破坏程度普遍有所提高；二是各个级别破裂区的分布范围相应地扩大了；研究区应力分布表现出明显的不均匀性，特别是剪应力，无论是O〓～S～D时期，还是C～P时期，都有很大的差异性，特别是在小断层的端部，剪应力比较集中，而且在断层的两盘，剪应力方向和大小都变化极快。
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The core of this model is using solid element to simulate elastoplasticity deformation of faultage and using contact element to simulate the interface of faultage and rock, and so, realizing the problems coupling of elastoplasticity and contact.
模型的核心是以三维实体单元模拟断层或软弱夹层材料弹塑性变形特性，以接触面单元模拟断层或软弱夹层与完整岩石之间交界面的力学特性，即剪切效应和法向提离效应，从而实现了弹塑性问题和接触问题的耦合。
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There are five types of deformational structure in the front zone of the Tang－Lun nappe, Ningzhen Mountain:great rotating of beds and imbricated system;reversed structure;transverse and oblique faults with the character of tear faults;warping of recumbent folds and kink band with advantageous shearing direction.
发育在宁镇山脉的汤―仑推覆体前锋带上的变形构造存在五种型式：岩层的大幅度旋转与密集的叠瓦系；反冲构造；具捩断层性质的横向及斜向断层；平卧褶曲的翘起和具优选剪切方位的膝折构造。
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The Altun fault, a famous tremendous sinistral strike-slip fault in NW China, is composed mainly of the Altun,master fault several secondary subhorizontal, sinistral, strike-slip faults and oblique faults.
阿尔金走滑断裂带主要由阿尔金主干断层与几条近于平行的左行走滑断层和斜交断层组成，其空间分布规律可用左行走滑简单剪切模型解释。
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Study on west Namco thrust Three ductile shear zones were discovered in Gayalong, Elongnubu and Shenjue-Gechangchayu, and geological features, deformation, motion direction and structural pattern are studied in detail for major thrust faults, ductile shear zones and folds in west bank of Namco Lake, leading to identification of west Namco thrust . And west Namco thrust and ophiolite mélanges outcropped from west Namco Lake to Yongzhuzangbu coexist together, indicating another tectonic suture in the Tibetan Plateau termed as the Namco-Yongzhu suture or NYS with its east extension to Jiali fault.
纳木错逆冲推覆构造研究：发现纳木错西岸嘎龙垭韧性变形带、饿弄怒布舍糜棱岩带和生觉—各昌茶玉韧性剪切带，详细观测典型逆冲断层的地质特征、变形特点、运动方向和序次关系，分析逆冲断层、褶皱构造、韧性剪切带的几何配置关系和动力学成因联系；分析纳木错逆冲推覆构造的空间影响范围，向东延伸与嘉黎逆冲断裂相连接，向西延伸与果忙错—永珠藏布构造带相归并，与纳木错西岸蛇绿岩、永珠藏布—果忙错蛇绿岩共同组成拉萨地块中部最重要的区域构造，命名为纳木错—永珠缝合带。
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According to the stress characteristics of coal floor with faults, corresponding simplified mechanical model is built to obtain the equations of shear stress and normal stress on the fault, as well as the influential rules of fault dip on shear stress, normal stress and fault activation.
针对含断层缺陷底板的受力特征，建立相应的简化力学模型，分析得到断层面上的剪切应力和法向应力表达式，并研究断层倾角对断层面上剪切应力、法向应力及断层活化的影响规律。
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Home position shear tests of slope rock, point loading tests and indoor AMD simulation action tests in XingQiao concave slope had show shearing strength and coherence between body layers of quartz sandstone decrease by 13.2%~21.3% after attacked by AMD, the angle of internal friction between layers is decreased by 5.0%~7.5%, in general, AMD affects the rocks mechanical property at range of 60~100m interior the perpendicular slop. Data analysis shows: 1 The actions to slope are major focused on zone of weakness, shearing strength of slope foot and AMD centre are reduced by 52% and 64.7% separately. 2 The explosion stress wave of long distance field has obviously increasing influence to disturbance amplitude value of slope with increasing of the slope height and distance, the response of the top of slope and fault region are obvious as well as damage effect; the foot of slope is with smallest disturbance amplitude value, the disturbance amplitude value of the step close to free face is obviously bigger than the interior of slope. 3 With the coupling effect of the AMD and explosion loading, the stress distribution inside of slope mainly presents characters of explosion stress field; the area affected by AMD becomes a weak area of shearing stress.
新桥深凹露天矿边坡岩体的原位剪切试验、点载荷试验、室内模拟AMD作用试验表明：AMD蚀化后的石英砂岩，岩体层面间的抗剪强度和粘聚力减小的幅值约为13.2%~21.3%；层面间内摩擦角减小幅值在5.0%~7.5%之间；AMD一般影响垂直边坡体内部在60~100m范围内的岩体力学性质数值分析表明：AMD对边坡体的作用主要集中在弱化区域内，边坡体的底脚和AMD作用中心区域的剪切应力减少了52.0%和64.7%；(2)随着边坡体高度和距离的增加，远场爆炸应力波对边坡扰动幅值的增加趋势明显，边坡顶部和断层部位的响应突出，损伤效应明显；边坡底脚扰动幅值最小，临空面附近台阶的扰动幅值明显大于边坡体内部；(3)AMD与爆破荷载耦合作用后，边坡体内部的应力分布主要呈现出爆炸应力场的特征，AMD影响区域形成了一个剪切应力弱区。
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The detachment fault zone is a low temperature shear zone with top to the E to SE extensional shearing and has typical S-L mylonites with both shearing and flattening strains.
拆离断层带是一个上盘向E到SE伸展剪切的低温剪切带，由具有剪应变和压应变的典型SL糜棱岩构成。
- 更多网络解释与剪断层相关的网络解释 [注：此内容来源于网络，仅供参考]
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antithetic fault：反向断层
antithetic conjugate Riedel shears 里德尔对偶共轭剪切 | antithetic fault 反向断层 | antithetic shear 对偶剪切
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antithetic shear：对偶剪切
antithetic fault 反向断层 | antithetic shear 对偶剪切 | antithetic slip cleavage 相向滑动劈理
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joist shears：型钢剪切机, 钢梁剪切机
hippomanic 有爱马癖的 | joist shears 型钢剪切机, 钢梁剪切机 | closed fault 闭合断层
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shear zone：剪裂带
有时断层带内可能还出现一组与断层大略平行的剪裂带(shear zone). 断层泥不具透水性,常阻滞地下水流而增加局部之地下水压,降低断层带之剪力强度,容易发生滑动. 同时断层带多由松软且破碎之物质组成,除强度较弱外,也容易被压缩,
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sinistral fold：左旋褶皱
sinistral fault 左旋断层 | sinistral fold 左旋褶皱 | sinistral shear fault 左旋剪切断层
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sinistral fold：左移褶皱
左移断层 sinistral fault | 左移褶皱 sinistral fold | 左移剪切断层 sinistral shear fault
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bedding-plane thrust fault：顺层冲断层
bedding-plane shear surface 层面剪切滑面 | bedding-plane thrust fault 顺层冲断层 | bede 丁字镐;鹤嘴锄
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shear thrust fault：剪冲断层
剪切触变性 shear thixotropy | 剪冲断层 shear thrust fault | 横波传播时间 shear transit time
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scissors fault：旋转断层
scissor tongs 剪式大钳 | scissors fault 旋转断层 | scissors 剪刀;剪形装置
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shear wave：剪切波
一般来说,P.S测井可原位测定压缩波(Pressure Wave)和剪切波(Shear Wave)在岩(土)体中的传播速度,从而避免了室内测试所带来的误差,它能有效地解决许多地质问题,诸如确定场地土类型、建筑场地类别;提供断层破碎带、地层厚度、固结特性和软硬程度、评价岩(土)体质量等;