fault movements meaning in Chinese
断层运动
Examples
- Ma jin and ma shengli , 1987 , the role of fault material in fault movement and seismological significance , earthquake research in china , 1 , 3
马胜利，马瑾， 1988 ，高温高压下石英和方解石断层带的摩擦滑动性状，地震学报, 10 , 1 。 - To extend takada ' s shell method , a 3 - dimension shell - spring fem is proposed to analyze the response of steel pipelines under the large fault movement in the second chapter
根据以上的研究背景，本论文采用壳模型有限元方法对管子在断层作用下的地震反应进行了分析。 - A physical model for describing the fault movement along plate boundary is proposed , i . e . , the crust movement along plate boundary equals to the relative rigid plate motion plus negative dislocation distributions on the fault planes
提出了一种描述板块边界断层运动的力学模型，即将板块边界的地壳运动表述为板块的相对刚体运动加边界断层面上的负位错分布。 - Compared with the beam model , the shell - spring model proposed in this paper can examine the failure mode of a buried pipeline under the fault movement more clearly . the occurrence of the third damage in thames water pipeline is specially discussed in chapter 3
在模拟土耳其地震大口径钢管的震害中，本文壳模型的分析结果与eidinger的梁单元模型比较，可以更清楚地解释管子第三处破坏产生的原因。 - The main conclusions are as follows . cross - fault displacement observation can directly reflect the recent activities of the major faults in the region . present fault movement and earthquake activity have a temporal correspondence with each other , they all show alternately quiet and active periods . the intensity of fault movement is a manifestation of the strength of regional principal compressional stress , it also indicates the strength of an earthquake in preparation
认为： 1 )跨断层位移观测资料能够直接反映区内主要断层的最新活动情况； 2 )断层现今活动与地震活动在时间序列上相互对应，均有活跃期与平静期相互交替出现的活动特徵； 3 )断层活动强弱是区域主压应力强弱的表现，亦是孕震强度的标志。