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fault mechanics
相关语句
  断层力学
     Study on Fault Mechanics Model and Numerical Simulation Methods
     断层力学模型及其数值模拟方法评述
短句来源
     This paper mainly outlines the new progress made in plate motion,lithostatic stress field,fault mechanics,active structure and long-term earthquake prediction.
     文章主要对板块运动、岩石圈应力场、断层力学、活动构造、长期地震预测方面的新进展做了概略介绍。
短句来源
     earthquake source modellingand fault mechanics;
     地震的震源模拟和断层力学
短句来源
     Fault mechanics models and numerical simulation methods often used in geology and rock mass mechanics are summarized and compared, and the current research situation and development trend are reviewed in this paper.
     对地学及岩体工程中常采用的断层力学模型及数值模拟方法作了简要的总结与比较,并对其研究现状及发展趋势做了述评。
短句来源
     Based on the e-valuation on many research cases, the sealing mechanism of lower-class faults and the dominant factors controlling sealing property were studied. A three-stage e-valuation method was summarized based on structural style analysis, which includes evaluations of the fault mechanics, the fault plane, the stratum arrangement and activity time arrangement.
     在大量的评价断层封堵性实例的基础上,研究了低序级断层的封堵机理以及控 制封堵性的关键因素,总结出基于构造样式分析的断层力学研究评价、断层面评价、地层配置与活动时间配置评价 的三级评价方法。
短句来源
  “fault mechanics”译为未确定词的双语例句
     A PRELIMINARY APPROACH TO THE IDENTIFICATION OF FAULT MECHANICS ACCORDING TO SEISMIC PATTERNS
     根据地震波形的变化特征鉴定断裂力学性质的初步探讨
短句来源
     So the fault symptoms of transformer are various, and the relation between the fault symptoms and fault mechanics is also complicated, which make it very difficult to establish a universal fault diagnosis method for transformer.
     由于变压器故障的复杂性,其诊断过程不可能只采用单一方法,而要采用多种方法。 因此,必须从各种学科中广泛探求有利于故障诊断的原理、方法和手段,这就使得故障诊断技术呈现多学科交叉这一特点。
短句来源
     So, it is a research hotspot to analyze its statics and dynamics, to find its inner fault mechanics and diagnose its fault.
     以轴对称问题的有限元分析为基础、ANSYS为计算机为工具,建立圆柱滚子滚动轴承有限元分析模型,对其进行了静力分析和模态分析,找出其故障机理;
短句来源
     Based on the fault mechanics and activity, bay formed mechanism, water system distribution, crustal deformation and GPS observations and others, the curent geodynamics enviroment in the Taiwan Straits and its both coasts is contrasted and studied.
     本文根据断层的力学性质、活动习性、褶皱、断陷盆地、平原、海湾的形成机理,火山活动、水系分布格局,震源机制解、地壳形变场、GPS观测成果和EDM(光电测距)资料等,对比研究了台湾海峡及其两岸现今的地球动力学环境。 结果表明:台湾海峡处在北西方向引张的应力环境;
短句来源
     By using the theory of fault sealing property the author has studied the fault sealing properties of two group fault systems which intersect vertically each other in this area from the two respects of fault mechanics and the relationship of lithology juxtaposition.
     运用断层封闭性理论 ,从断层的力学机制和断层两侧的岩性配置关系两个方面剖析了永 8地区相互正交的两组断裂系统的封闭性。
短句来源
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  fault mechanics
This may have implications for fault mechanics as well as for aspects of shaking hazard near faults.
      
We review studies on fault zone structures in land areas and fault mechanics studies related to the fault zones.
      
The interaction of pore fluids with fault mechanics is an especially interesting and critical part of this work.
      
The episodicity of a fault is an important element in fault mechanics, with some fault zones recording 1000-2000 individual episodes.
      


The author puts forward that we should take active structure related to earthquakes as the main study object in seismogeologieal research.In recent four years we have made important progress in fields of seismogeological study.This paper mainly outlines the new progress made in plate motion,lithostatic stress field,fault mechanics,active structure and long-term earthquake prediction.Finally,the paper,based on the developments in this study field in the world and integrating with actual conditions in China,raises...

The author puts forward that we should take active structure related to earthquakes as the main study object in seismogeologieal research.In recent four years we have made important progress in fields of seismogeological study.This paper mainly outlines the new progress made in plate motion,lithostatic stress field,fault mechanics,active structure and long-term earthquake prediction.Finally,the paper,based on the developments in this study field in the world and integrating with actual conditions in China,raises some personal ideas of the key points and direction of future research in seismogeology in China.

本文作者提出,地震地质学研究内容应以与地震有关的活动构造为主要研究对象。近4年来,地震地质学研究在多方面取得了重要进展。文章主要对板块运动、岩石圈应力场、断层力学、活动构造、长期地震预测方面的新进展做了概略介绍。最后,根据国际研究动态,结合我国实际情况,对我国地震地质学今后研究重点和方向提出了几点个人思考意见,供有关方面参考。

The 27th General Assembly of IASPEI was held at Victoria University of Wellington,Wellington,New Zealand,from10-21 January 1994.The Assembly was attended by 483 scientific participants from42 countries.The State Seismological Bureau sends a 13-member delegation headed by Prof.chen Rong,deputy director of the SSB to the Assembly.The Assembly organlzed 27 symposia and workshops,with 399oral papers and about 160 posters presented.The symposia and workshops of the IASPEI General Assembly dealt with extensive frontier...

The 27th General Assembly of IASPEI was held at Victoria University of Wellington,Wellington,New Zealand,from10-21 January 1994.The Assembly was attended by 483 scientific participants from42 countries.The State Seismological Bureau sends a 13-member delegation headed by Prof.chen Rong,deputy director of the SSB to the Assembly.The Assembly organlzed 27 symposia and workshops,with 399oral papers and about 160 posters presented.The symposia and workshops of the IASPEI General Assembly dealt with extensive frontier problemsof seismological and geophysical studies,including:wave propagation in heterogeneous media──deter-ministic and stochastic;earthquake hazard and risk;sedimentary basins of the Asia-Pacific region and theirtectonic setting;deep earth discontinuities──configuration and dynamics;earthquake prediction;seismictomography and mantle dynamics;subduction zone and back arc basins;geothermal aspects of lower cruststructure,petrology and rheology;location and quantification of regiornal earthquakes;milli-and micro-Hzseismology;detailed seismic studies in ridge areas;seismological and tsunami hazards in the Pacific;anisotropy on large and small scales;upgrading global seismological practice;earthquake source modellingand fault mechanics;induced seismicity;non-linear seismology;effects of surface geology on seismic mo-tion;space geodesy and real time tectonics;heat flow and hydrothermal circulation;broad-band seismologyand seismic sources etc.

国际地震学与地球内部物理学协会(LASPEI)第27届大会于1994年元月10-21日在新西兰首都惠灵顿的惠灵顿维多利亚大学举行。来自42个国家的483位科学家参加了这次大会。国家地震局派出了以副局长陈为团长的13人代表团出席会议。本届大会共安排了27个学术报告会和研讨会,会上宣读论文和报告399篇,张贴展示论文约160篇。本届IASPEI大会的学术报告会和研讨会涉及广泛的地震学和地球内部物理学研究的前沿问题,内容包括:波在非均匀介质中的传播;地震危险性与地震危害;亚太地区的沉积盆地及其构造背景;地球深部间断面的构造形态和动力学;地震预测;地震层析成像和地幔动力学;俯冲带和弧后盆地;地热在下地壳、岩石学与流变学等方面之作用;区域地震的定位和定量化;毫赫与毫微赫地震学;脊区的地震学详细研究;太平洋的地震和海啸危险性;大小尺度的各向异性;全球地震观测技术的改进;地震的震源模拟和断层力学;诱发地震;非线性地震学;地震运动的地面地质效应;空间大地测量学和实时构造地质学;热流和热液循环;宽频带地震学和震源,等等。

Based on the fault mechanics and activity, bay formed mechanism, water system distribution, crustal deformation and GPS observations and others, the curent geodynamics enviroment in the Taiwan Straits and its both coasts is contrasted and studied. The results show that the Taiwan Straits is in the strain cirumstance extended by the westnorth direction, the Taiwan region is compressed by the westnorth direction from the Pacific Ocean-Philippine Plate and the eastsouth direction from the descending of Taiwan...

Based on the fault mechanics and activity, bay formed mechanism, water system distribution, crustal deformation and GPS observations and others, the curent geodynamics enviroment in the Taiwan Straits and its both coasts is contrasted and studied. The results show that the Taiwan Straits is in the strain cirumstance extended by the westnorth direction, the Taiwan region is compressed by the westnorth direction from the Pacific Ocean-Philippine Plate and the eastsouth direction from the descending of Taiwan Straits, and the Fujian inshore is compressed by the east and north direction from the lndian Plate, the westnorth direction from the Pacific Ocean Philippine Plate and the westnorth direction from the descending of Taiwan Straits.

本文根据断层的力学性质、活动习性、褶皱、断陷盆地、平原、海湾的形成机理,火山活动、水系分布格局,震源机制解、地壳形变场、GPS观测成果和EDM(光电测距)资料等,对比研究了台湾海峡及其两岸现今的地球动力学环境。结果表明:台湾海峡处在北西方向引张的应力环境;台湾地区受到来自太平洋菲律宾海板块向北西方向的挤压和因台湾海峡下降而产生的向南东方向的挤压;福建沿海则受到印度板块向北向东的挤压和太平洋菲律宾海板块向北西方向的挤压以及台湾海峡下降而产生的向北西方向的挤压。

 
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