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left-lateral motion
相关语句
  左旋走滑运动
     The earthquake rupture in frozen soils mainly shows brittle deformation, and is composed of shear fractures, tension fractures and seismic ridges caused by the left-lateral motion of the seismic fault.
     冻土中地震破裂带在地表主要以脆性变形为主 ,在地震断裂左旋走滑运动作用下 ,主要由剪切裂缝、张裂缝和开裂的挤压鼓包等组成。
短句来源
  “left-lateral motion”译为未确定词的双语例句
     And it is indicated that Western Guangxi is under an action of principal compression stress trending approximately EW or WNW-ESE direction since Ceno-zoic era, which results the NW striking fault zone featuring a left-lateral motion and showing a typical tectonogeomorphology of strike-slip fault zone.
     指出新生代以来,桂西地区受到近东西向或北西西—南东东向主压应力的作用,使北西走向的右江断裂带作左旋走滑为主的运动,形成了走滑断层所具有的典型的构造地貌形态。
短句来源
     Using various horizontal deformation network data of the Study Are, the basic characteristics of regional stress field in middle and north section of the Honghe Fault are obtained. (1) Northern area is of tensional left-lateral motion type. (2)Middle area is of compressive left-lateral motion type.
     利用场区各种类型水平形变网数据,求得红河断裂中、北段的区域应力场基本特征是:(1)北区为张性左旋型,(2)中区为压性右旋型,(3)南区为张性右旋型。
短句来源
  相似匹配句对
     two were left .
     右肩8例,左肩2例。
短句来源
     left noether;
     左Coherent环;
短句来源
     Left C-a Semigroups
     左C-a半群(英文)
短句来源
     ON LEFT POSITIVELY. TO. -SEMIGROUPS
     关于左正定t.0-半群
短句来源
     There are lateral fins on the flagellum.
     鞭毛上有侧鳍。
短句来源
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  left-lateral motion
Left-lateral motion between the Pacific and Bismarck plates appears to drive the counterclockwise pivoting motion of the Manus microplate and the complementary wedge-like opening of the MSC and the Southern Rifts.
      
At 95% confidence, the slip rate estimate falls between 7?mm/year of left-lateral motion and 15?mm/year of right-lateral motion.
      


Based on the practical data from field survey in recent years, this paper makes a summary on neotectonic characteristics of Youjiang active fault zone. And it is indicated that Western Guangxi is under an action of principal compression stress trending approximately EW or WNW-ESE direction since Ceno-zoic era, which results the NW striking fault zone featuring a left-lateral motion and showing a typical tectonogeomorphology of strike-slip fault zone. In addition, earthquake activity along this fault zone...

Based on the practical data from field survey in recent years, this paper makes a summary on neotectonic characteristics of Youjiang active fault zone. And it is indicated that Western Guangxi is under an action of principal compression stress trending approximately EW or WNW-ESE direction since Ceno-zoic era, which results the NW striking fault zone featuring a left-lateral motion and showing a typical tectonogeomorphology of strike-slip fault zone. In addition, earthquake activity along this fault zone is also discussed.

本文根据近年来野外考察的实际资料,总结了右江断裂带的新构造活动特征。指出新生代以来,桂西地区受到近东西向或北西西—南东东向主压应力的作用,使北西走向的右江断裂带作左旋走滑为主的运动,形成了走滑断层所具有的典型的构造地貌形态。此外,对右江断裂带的地震活动进行了讨论。

Post mid-Cretaceous sedimantary basins developed on the northern marginof the South China Sea display unique characteristics in their spatial and tem-poral distribution. Three basin evolutionary cycles which started in Late Creta-ceous, Late Eocene and Middle Miocene respectively, have been recognized.Each of the cycles resulted from a seperate rifting episode. Interestingly,orien-tations of the major trends of the basins varied from predomenantly NE forthe first cycle through NE-EW for the second to EW-NW for...

Post mid-Cretaceous sedimantary basins developed on the northern marginof the South China Sea display unique characteristics in their spatial and tem-poral distribution. Three basin evolutionary cycles which started in Late Creta-ceous, Late Eocene and Middle Miocene respectively, have been recognized.Each of the cycles resulted from a seperate rifting episode. Interestingly,orien-tations of the major trends of the basins varied from predomenantly NE forthe first cycle through NE-EW for the second to EW-NW for the third. Conse-quently, the early configuration of an individual basin has been apparentlysuperimposed by the later events, resulting in a very complex pattern. Mechanical analysis suggests that the NE trending basins of the first cycle were probably the result of rifting along the extensional direction in a NWtensional terrane, whereas the NE-EW and EW-NW couples of the second andthird cycles can be best explained by extension along Riedel shear and tensionalcomponents under a sinistral divergent wrench regime whose azimuth has rotatedclockwise through time. Therefore, major changes in regional stress field areindicated. The tectonic setting related to the first basin cycle is inferred to be a intra-arc ard back-arc extensional domain induced by dip-steepenning of subductedoceanic slab when the convergence rate between Pacific and Eurasian Platesdecreased in Late Cretaceous. The collision of Indian Plate with Eurasian Plateabout 40 m.y. ago and the following penetration of the former into the laterled to the large left lateral motion along Red River Fault and the clockwiserotation of Indochina as Indochina block and South China block were extrudedsuccessively by the collision, thus initiating the second and third basin evolu-tionary cycles.

南海北部边缘自晚自垩世以来有过三个成盆期,盆地的走向发生了顺时针的旋转,这种演变是由特定的大地构造环境所决定的。在40百万年以前,盆地发育与太平洋和欧亚板块聚敛边缘有关,属弧间和孤后扩张性质;之后,则主要由印度板块与欧亚板块碰撞引起的陆壳沿红河断裂带的走向滑动和印支地块的顺时针旋转所控制。

Using various horizontal deformation network data of the Study Are, the basic characteristics of regional stress field in middle and north section of the Honghe Fault are obtained. (1) Northern area is of tensional left-lateral motion type. (2)Middle area is of compressive left-lateral motion type. (3)Southern area is of tensional right-lateral motion type. The regional stress field of this area is dominantly tensional and the compressive left-lateral motin type in mid-area just reflects...

Using various horizontal deformation network data of the Study Are, the basic characteristics of regional stress field in middle and north section of the Honghe Fault are obtained. (1) Northern area is of tensional left-lateral motion type. (2)Middle area is of compressive left-lateral motion type. (3)Southern area is of tensional right-lateral motion type. The regional stress field of this area is dominantly tensional and the compressive left-lateral motin type in mid-area just reflects the partial characteristics of stress field in the transform area. In the North primary strain accumulation and its rate is larger than in the S-area. The maximum strain accumulation is in Jianchuan and the high-sensitive area in Houshan Dingxiling.Based on horizontal deformation data the calculation and analysis of deformation and strain in the srudy Area result in the parameters of recent principal active tectonics. By use of precursory deformation information and post-seismic effect some earthquakes are analysed and the potential source zones in 3-5 years are pre-estimated.

利用场区各种类型水平形变网数据,求得红河断裂中、北段的区域应力场基本特征是:(1)北区为张性左旋型,(2)中区为压性右旋型,(3)南区为张性右旋型。场区区域应力场基本以张性为主,中区的压性右旋型恰好反映转换区应力场的局部特征。北区主应变积累和速率比南区大,最大处在剑川,而高敏感区在后山定两岭。基于水平形变和应变分析,获得了场区现今主要活动构造参数。利用地震前兆形变信息和震后效应进行了地震震例分析。并对3~5年内的潜在震源区进行了预估。

 
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