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fault dip相关的网络例句

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与 fault dip 相关的网络例句 [注:此内容来源于网络,仅供参考]

The research results indicate that (1) fault-failure-type water inrush occurs more often than floor-failure-type water inrush under the existence of normal fault;(2) the influence of fault step and dip angle on the feature and position of water inrush is not evident, and water inrush may occur at both coal layer and the floor near working face;(3) the distance of coal column for preventing water inrush should be increased with the increase of fault step and dip angle.

得出以下结论:(1)当存在正断层时,多发生断层破坏型突水,而底板破坏型突水发生的几率较小;(2)突水性质和突水发生位置受断层断距和倾角的影响不大,煤层和采煤工作面附近的底板围岩都可能成为突水涌出点;(3)随着断层断距和倾角的增加,防水煤柱的合理留设距离应随之增大。

Figure 6 Schematic of a thrust fault (dip slip fault with landmasses coming together).

地震摇晃对于盆地和山脉内部来说,都是破坏性的。

Figure 6 Schematic of a thrust fault (dip slip fault with landmasses coming together).

Figure 6 插入式断裂带(侵入式滑断层与大陆碰到一起)示意图。

The numerical simulation reveals the formation principle of water inrush channel in coal floor with fault structure as well as influential rule of fault dip on water inrush in coal floor.

模拟结果在一定程度上揭示含断层构造底板突水通道的形成机制及断层倾角对底板突水的影响规律。

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。

According to systematic numerical simulation test, it studies the influences of four primary factors of fault: thickness, fault dip, fault deformation modulus and lateral pressure coefficient of initial stress.

通过系统的数值仿真试验来研究断层厚度、断层倾角、断层弹模、地应力侧压系数等四个主要因素的影响。

Without considering surface covering layer, the surface earthquake dislocation and strain distribution near active fault were calculated under different conditions of magnitude, fault movement style and fault dip angle using 3-D finite element method. Based on above results, the safe distance of active fault to important project site was studied.

:在不考虑地表覆盖层的情况下,采用三维有限元方法计算了不同震级、不同断层活动方式以及不同断层倾角下断层上、下盘地表的地震位移及形变分布,通过设定的安全距离判定标准,研究了各种情况下工程场地距断层的安全距离。

In this paper,the authoruses the method of the explicit finite-element numerical simulation, which isbased on the most simple two-dimensional-finite-element modle and kinematicsource model,to study the basic characteristics of near-fault ground motion, suchas the changing tendency of the hanging-wall effect and the vertical effect as weonly change the fault dip or the depth of the top of the fault.

本文拟利用最简单的二维有限单元模型和基于有限断层假定的震源运动学模型,采用集中质量显式有限元数值模拟的方法研究近断层地震动的特征,如上盘效应和竖向效应随断层倾角以及断层的上界埋深的变化而改变的趋势。

Results show that many geological phenomena,surface ruptures,change of fault dip angle,vertical displacement of two plates alone fault and distribution of huge geo-hazards,are highly related with D-InSAR image.

基于差分干涉雷达观测及相关资料,对龙门山断裂在本次地震中活动性进行了初步分析,结果表明干涉雷达形变图像与地表破裂范围、逆冲角度的变化、上下盘升降关系及大型余震的展布存在很强的相关性。

In this paper, some improvements have been made on the traditional gradient interpretation methods for the two-dimensional fault gravity anomalies:① The least squares fitting technique is adopted to figure out the dip angleαof the step;② The dip angle and the horizontal boundary of the step are directly used to calculate the burial depth of the step;③ the interpretation method for gravity two-dimensional gradient is extended to the interpretation of the complex fault model.

摘要对以往的二维断裂重力异常的梯度解释方法作了几点改进:①采用最小二乘拟合方法求取台阶倾角α;②直接利用台阶倾角与台阶的水平边界位置来计算台阶的埋深;③将重力二维梯度解释方法推广到复杂断裂模型的解释。

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