英语释义

1. a fault about which movement is predominantly horizontal

2. a slipping movement along the strike of a fault
strike-slip earthquakes

片语

strike-slip active走滑活动

strike-slip characteristics走滑特征

strike-slip shear走滑剪切

strike-slip basins走滑盆地

strike-slip duplex走滑双重构造

strike-slip motion走滑运动

strike-slip inversion走滑反转构造

strike-slip processes走滑作用

strike-slip tectonic走滑构造

英汉例句

• The vertical movement strength and deformation status evolve with time. The horizontal movement and deformation show obvious compressional strike slip character.

  垂直差异运动强度和变形态势随时间演变，水平运动与变形呈明显的挤压走滑特征。

• Earthquake nucleation with strike slip fault was analyzed by means of the variational boundary integral method and slip weakening friction law.

  利用边界单元法和滑移弱化摩擦本构关系分析了平移断层上地震的产生。

• The strata form and quasi strata form ore bodies are controlled by strike slip faults.

  矿体受层滑断层控制呈层状、似层状。

• Some large strike slip faults, such as the Xianshuihe fault, consist of main fault and several sub-faults, which are commonly arranged as en echelon (or parallel) pattern.

  大的走滑断裂带，如鲜水河断裂，是由主干断裂及与其相伴的若干阶式（或平行）断裂组成。

• If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.

  如果断层走向与区域构造的总体走向相平行，就称之为纵向断层；

• The main type of fracture are tensional fault, compressional fault and strike slip fault.

  断裂的类型主要有拉张或张扭断层、拉压或压扭断层、走滑断层。

• A complete suit of closely analytical expressions of stress field is presented for the strike slip shear fault with an arbitrary dip Angle in a semi infinite medium.

  给出了半无限空间中任意倾角的走向滑动剪切断层错动产生的应力场的一套严密的解析表达式。

• The oblique strike slip structure is resulted from the closing of little Jingshajiang regeneration ocean basin and the oblique intercontinental collision in late Triassic.

  滇西北拖顶地区斜向走滑构造是金沙江再生小洋盆关闭、陆-陆斜向碰撞构造转化的结果。

• The Paleogene tectonic framework in Bohai Bay was controlled by both Mesozoic sinistral strike slip and Paleogene extension resulted from diapiric intrusion of mantle.

  中生代左行走滑和早第三纪伸展作用共同控制了渤海海域早第三纪的构造格局。

• These factors include district cap rock, strike slip properties, the intensities of fault activity and the distance from oil source.

  研究结果表明，区域盖层、走滑性质、断层的活动强度、油源的充足程度是油气纵向分布的主要控制因素；

• Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area, this paper suggests that Fangzheng rift is a rifted basin formed by strike slip pull apart.

  本文通过对方正地区所发现的负花状构造及其有关构造运动形迹分析的基础上，进一步提出方正断陷是走滑—拉分形成的断陷盆地。

• The formation time of NE strike slip faults is earlier than that of NW strike slip faults.

  另一组为NW向走滑断层，形成时代较晚，破坏早期逆沖断层和NE向走滑断层。

• The secular GPS crustal deformation image has reflected the relatively complete left lateral strike slip movement of this active fault zone.

  长趋势GPS地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动。

• The analyses of regional structures show that Lianyunshan granite is associated with dynamic metamorphism shear remelt magmatism of NNE trending convergent strike slip faulting during t 3-j.

  区域地质构造解析结果表明，连云山花岗巖与晚三叠世—侏罗纪nne向会聚走滑断层动热变质—剪切重熔型巖浆作用有关。

• In the after strike slip compressional stage, this lake was filled up with the clastic sediments of deltic and fluvial facies.

  在随后的走滑挤压阶段，该湖泊为三角洲和河流相碎屑沉积物充填。

• According to the analysis of Mesozoic and Cenozoic tectonic evolution, Bohai Bay basin is a strike slip pull apart basin formed in the Cenozoic Eocene epoch.

  从渤海湾盆地的中、新生代构造演化分析，渤海湾盆地是一个新生代早第三纪始新世形成的走滑拉分盆地。

• In Longling fault zone and the area north to it, the direction of maximum compressional stress is near NS or NNW, the stress regime is of strike slip type.

  龙陵断裂带及其以北的局部地区，最大主压应力方向为近南北或北北西，应力结构为走滑型。

• The faults are mainly of reverse and strike slip faults, with a few synsedimentary normal, decollement and reversed faults.

  断裂以逆断层和走滑断层为主，还有少量的同沉积正断层、滑脱断层、反转断层等。

• If the relative movement of hanging wall and footwall is parallel to the strike of fault plane it is a strike slip fault.

  如果断层上盘和下盘的巖石相对位移运动是平行断层面走向的，这种断层称为走滑断层。

• The focal mechanism of the M4.9 earthquake shows that it belongs to strike slip type that is similar to the M6.4 earthquake in 1969.

  本次4.9级地震作出的震源机制解显示为走滑型，与1969年主震的情况较为类似。

• The lower-order faults were formed under the action of strike slip stress, extension stress, camber stress and traction of master faults.

  低级序断层是在走滑应力、伸展应力以及受主断层的牵引或在局部地区的拱升应力等作用下形成的。

• The distribution of slip displacement, slip velocity and friction force on the strike slip fault were obtained by numerical simulation.

  通过数值计算得到了平移断层上滑移位移、速度及摩擦力的分布规律。

• It indicates that two dynamical mechanisms of mantle diaper and right-lateral strike slip in deep faulted zone lead tectonic dynamics model evolved in Cenozoic stress field of Dongpu depression.

  提出了地幔底辟和深断裂带右旋走滑位移两种动力机制联合作用主导了东濮凹陷的新生代应力场演化的构造动力学模式。

• The study shows that volcanic activity in Xiangshan volcanic basin may be divided into two cycles, and its emplacement is controlled by strike slip pull apart process originated from the deep regiona.

  研究表明 ，相山火山盆地火山活动划分为两个旋回 ，其就位受制于区域深断裂的走滑拉分作用。

• In this paper, a method, the uniform slip method, estimating average slip rate along surface trace of strike slip fault zone by historical earthquake data is offered.

  本文介绍并完善了作者提出的一种根据历史地震资料估计走滑断裂带地表断层平均滑动速率的方法：「均一滑动法」。