查询词典 fault

Under the circumstances that some prior knowledge about the possible fault can be obtained,the dynamic behavior of the fault is proposed and used to solve fault estimation problem.While,if there is no extra knowledge available about the possible fault other than the condition of l_2 bounded,the residual generation is formulated into a problem of observer-based H_∞filtering problem in the sense of stochastic,and the linear matrix inequality approach to solve this problem is proposed.

对于能够了解部分故障先验知识的情况，提出描述故障结构特性的动态模型，解决H_∞故障估计问题；而当故障信息完全未知情况下，将基于观测器的残差产生器设计归结为随机意义下的H_∞滤波问题，提出了该问题求解的线性矩阵不等式方法。

This study shows that there are 4 kinds of volcanic facies in deep volcanics in north Songliao Basin: eruptive facies, overflow facies, volcanic vent facies and volcanic sedimentary facies. There are 4 volcanic eruption cycles: Huoshiling period, Shahezi period, Yingchengzi period and Quantou period. There are 4 structural evolution stages: north-south accumulation, west-east subduction, uplift mantle and thin crust, alternative open and close. There are 4 kinds of pool-forming patterns:(1) pattern with the migration along the unconformity and fault to the near crater;(2) pattern with the migration along unconformity and fault to the rift margin;(3) pattern with the migration along unconformity, fault and fracture to the source rock;(4) pattern with the migration of the deep gas along the deep and large fault to the volcanic trap.

研究认为，松辽盆地北部深层火山岩主要存在四种火山岩相：即爆发相、溢流相、火山通道相、火山沉积相，划分为四个火山喷发旋回：即火石岭期、沙河子期、营城子期、泉头期，经历了四个构造演化过程：即南北夹攻、东西俯冲、幔隆壳薄、开合交替，具有四种成藏模式：即沿不整合面和断层运移至近火山口处火山岩圈闭聚集成藏模式、沿不整合面和断层砂岩疏导层运移至断陷边部火山岩圈闭聚集成藏模式、沿不整合面及断层、裂缝运移至源岩区内凹中隆火山岩圈闭聚集成藏模式、深部无机成因天然气沿深大断裂运移至火山岩圈闭聚集成藏模式。

The western part of the fault bundle-the Jintananshan Fault, tends to meet with the Kuantanshan Fault-the east part of the Altun Fault and has some relations to the Wenzhushan uplift in the transformation.

断裂束西段的金塔南山断裂与阿尔金断裂带东段的宽滩山段趋于交会，并与文殊山构造隆起之间构成构造转换关系。

In the field of liability without, negligence, causativeness of the parties action should be compared when only the injured party has fault. Causativeness of the dangerous element and fault element should be compared when both parties have fault. After should compare the degrees of fault of both parties, and at last definite in which degree to diminish the compensation liability of the injuring party.

在无过失责任领域内，当只有受害人过错时，应当比较双方行为的原因力；当双方均有过错时，应当比较危险因素与过错因素各自的原因力，在确定了过错因素的原因力后，再比较双方的过错程度，最终确定应在多大程度上减轻加害人的赔偿责任。

Currently, in the oil-field exploitation, existing the phenomenon of garbling the lack thickness of stratum with vertical fault-throw in well logging identification of strata while meeting fault in drilling well. In most case, consider the lack thickness of stratum which contrast the imperfection geologic strata thickness to the well and the well as the fault-throw. The method which using very popular in oil-field exist shortages, it very much easily lead people into the areas of misplay. especially when the seismic person and geology confirm the fault-throw, It often appear inconsistent instance.

目前，在油田开发中钻井钻遇断层时，地质人员时常存在将测井分层与相邻井对比时缺失地层厚度与铅直地层断距混淆的现象，很多情况下把井与井对比缺失地层厚度等同于断层断距等，这些现今在油田非常流行的用法存在一些不足之处，容易把人们引入一些认识上的误区，特别是在地震与地质人员进行断层断距的确定时，经常出现矛盾的情况。

Based on the systematic study of fault gouge characteristics (such as minerals component, granulometric composition structure and fractal, maturity, present activity and topotaxy by the SEM), a new way using microscopic and quantitative characteristics of fault gouge is put forward to evaluate the aseismatic problem and the fault resistance problem of concealed fault.

基于断层泥的特征（矿物组分、粒度成分结构和分形、成熟度和目前活动度和SEM特征等）的系统研究，探讨和提出了以断层泥的显微和定量特征来评价隐伏断裂的抗震和抗断难题的新思路和方法，并在镇扬大桥工程区域稳定性评价实际应用中取得了良好的效果，这对建在断裂带上的特大型桥梁工程的稳定性评价具有重大意义。

Because the uncertainty factors in network fault propagation model and the results of fault localization algorithm often cause the inaccurateness of the final diagnosis results, we propose a fault diagnosis solution which based on the L-best fault hypotheses.

针对网络故障传播模型和故障定位算法结果中不确定性因素导致最终诊断结果不准确的问题，提出了基于前L个最佳故障假设的故障诊断方案。

The results of rupture landform investigation indicate that this fault is one of weak active faults in Holocene, its average vertical slip rate is 0.5~0.6mm/a. On Jun. 15, 1975, Liuba M6.2 earthquake in Kangding occurred on the fault. The macro-epicenter located at Shuobu-Moda, Liuba county. The direction of long axis of meizoseismal area is same as that of Yunongxi fault trend. The occurrence of the earthquake is resulted from the newest activity of the fault.

断错地貌研究结果表明，该断裂为一条全新世弱活动断裂，平均垂直滑动速率为0.5~0.6mm/a左右。1975年1月15日康定六巴6.2级地震发生於该断裂上，宏观震中位置位於六巴乡溯布－莫达村附近，极震区长轴方向与玉农希断裂走向一致，是该断裂最新活动的表现。

Nextly, develop a fault diagnosis data collecting system which solved real-time dataacquisition in the power system fault diagnosis, the data message is analysed in detail andextract the data required in fault diagnosis, this system can not only collect data but alsotransmit the data information to attemper and provide a necessary condition for electric powersystem fault diagnosis On-line.

其次，开发电力系统故障诊断数据信息采集系统，该系统解决了电力系统故障诊断过程中故障特征信息很难实时获取的问题，同时对数据报文进行了详细的分析，提取出故障特征信息，该系统不但可以采集数据，而且还可以将数据信息实时传送至调度，为电力系统大规模在线故障诊断提供了必要的条件。

Hechi-Yishan fault zone is located in the north of Guizhong depression, which general strike is NW-EW and consists of a series of obduction fault. Generally, there are two main faults, the fault-fold belt about 5-20km is made of main faults, subsidiary faults and concomitant folds; The dip of main faults is N or S; It can be divided into four different structural sections along its strike (Hechi section, Yishan section, Liucheng section and Yingshan section). There are some differences among these sections in structure characteristic, such as fault structure, associated structure, fold association style, deformation of rock, and so on.

河池-宜山断裂带展布于桂中坳陷北部，总体走向NW-近EW 向，由一系列逆冲断层组成，主干断裂一般为2条，主干断裂与次级断裂及伴随的褶皱构造构成宽5-20km 不等的断褶带；主断裂倾向N 或S；沿走向可分为河池、宜山、柳城、英山四个构造段；各段断裂结构、伴生构造、褶皱组合样式、岩石变形等构造特征存在一定差异。

Liapunov—Schmidt method is one of the most important method in the bifurcation theory.

Liapunov—Schmidt方法是分叉理论的最重要方法之一。

Be courteous -- even when people are most discourteous to you .

要有礼貌──即使当別人对你最不礼貌的时候。