挤压作用的英文

• extrusion effect
• squeezing action

• "挤压"英文翻译    cirmp; squeeze; mouthpiece p ...
• "作用"英文翻译    act on; affect
• "外部挤压作用" 英文翻译 :    external loading
• "造山挤压作用" 英文翻译 :    orogenic crumpling
• "转子挤压作用" 英文翻译 :    rotor squish action
• "挤压作用；压实作用" 英文翻译 :    squeezing action
• "挤压作业" 英文翻译 :    squeeze job
• "冰静压作用" 英文翻译 :    cryostatic process
• "冲压作用" 英文翻译 :    ram effect
• "磁压作用" 英文翻译 :    pinch effect
• "减压作用" 英文翻译 :    decompressing effect
• "降血压作用" 英文翻译 :    hypotensive activity
• "刻压作用" 英文翻译 :    indentation
• "扩压作用" 英文翻译 :    diffusing action
• "气压作用" 英文翻译 :    pneumatic action
• "增压作用" 英文翻译 :    supercharging
• "波浪抽压作用" 英文翻译 :    wave pumping
• "水力楔压作用" 英文翻译 :    hydrailic wedging
• "无压作用时间" 英文翻译 :    pressure off time
• "在外压作用下" 英文翻译 :    under external pressure
• "计算风压作用力臂" 英文翻译 :    rated wind pressure lever
• "水压作用条件下" 英文翻译 :    under water head condition
• "在外压作用下纵向的" 英文翻译 :    longitudinal under external pressure
• "挤压变质作用" 英文翻译 :    compression metamorphism
• "挤压断裂作用" 英文翻译 :    compressional faulting

• It was primarily formed by undercompaction , hydrocarbon generation and tectonic compression
  柴北缘异常高压主要由欠压实作用、生烃作用及构造挤压作用形成。
• Lime - soil compaction piles of pile sinking compact the soil between them by lateral expanding when making holes
  灰土挤密桩是利用成孔时的侧向挤压作用使桩间土得以挤密。
• The inversion further shows that vertical loading on plate can produce significant affects on horizontal stresses
  反演结果也表明，除了过去公认的东西向挤压作用外，巴西还受到相当明显的南北向构造作用。
• In the late early cretaceous , the ncc turned into contraction stage again by the influence of the subduction of pacific plate and indian plate
  早白垩世晚期该区受太平洋板块和印度洋板块俯冲作用影响，华北板块再次转入挤压作用阶段，开始了滨太平洋域的演化。
• When tc approaches to coast , under the squeezing effect between tc and land , convergences of wind vector and pressure gradient are intensified between tc " s center and coast , and , a new high wind domain forms
  随着热带气旋不断接近陆地，由于挤压作用，二者之间区域的风矢量辐合和气压梯度不断增强，形成新的大风区，造成水平结构的变化。
• The multi - formation of chips often collects into groups and felts on the surface of concrete sawing area or segment , which will make the sawblade easy to be loaded under the extrusion of cement chips and diamond grits
  在粘性水泥粉屑以及金刚石磨粒的挤压作用下，多种形态的切屑易粘结成团，并粘附到混凝土锯切表面和锯片节块上而导致锯片堵塞。
• During subduction northward of neo - tethys oceanic plate , ayla - zhongba micro - continental , the marginal ocean basin and india continental drifted northward all together , the marginal ocean basin was gradually contracted and closed by compressed of india continental
  在新特提斯洋板块向北俯冲消减过程中，阿依拉仲巴微陆块、陆缘洋盆和印度大陆一起随着向北漂移，在印度大陆向北挤压作用下洋盆逐渐收缩以致最终闭合。
• The fault controlled the magmatism and metallization relevant to the contact zone , and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene . the fault zone deformed right - laterally under ne - sw striking transtention , and new joints zone was produced at the end of the two main faults because of local stress concentration . the fault produced inchoative cataclastic rocks , and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks , which was during the himalayan movement
  其后的继承性活动在断裂带内形成碎裂程度最强达到碎裂岩的碎裂岩系列构造岩，变形带两侧发育两组典型的共轭剪节理；第二次在晚白垩世?始新世，断裂在北东?南西向近水平挤压作用下右行张扭性活动，断裂带两主断裂在斜列重叠的端部由于局部应力集中进一步扩展形成节理带，而断裂在岩体区也发育两组典型的共轭剪节理，断裂内形成初碎裂岩为主的构造岩；第三次是喜山期以西侧抬升、东侧下降的强烈升降为主的活动，在基岩中，主断层两侧围岩出现微破裂。
• Those two phases of conjugated shear joints are differ from each other in spatial distribution , which is a reflection of the spatial evolution of the fault zone . it can beinferredfrom the information about macrostructure , superimposed deformation of tectonites , paleotectonic stress field of joints and other related documents that there had been three stages of significant activity since zijingguan fault zone was activated . the first stage was about from middle juiassic to early cretaceous , when the fault zone activated left - laterally under nw - se striking transpression
  宏观构造组合特征、构造岩变形叠加信息、节理的古构造应力场信息及前人区域资料表明，紫荆关断裂带自古生代末开始活化以来有三次主要构造活动：第一次是中侏罗世?早白垩世，在北西?南东向近水平挤压作用下，断裂左行压扭性活动，控制太行山地区岩浆岩带及与其相关的接触交代型矿床的形成。
• Under the strong compression from the orogenic belts on both sides , in the jurassic an atypical foreland basin developed on the southern margin of the qilian orogenic belt ; in the tertiary , a two - side foreland basin formed between the qilian orogen and kunlun orogen ; in the quaternary , the qaidam basin is a compressional , downwarped basin
  在两侧造山带的强烈挤压作用下，侏罗纪时期在祁连造山带南缘形成并不典型的前陆盆地，古近纪至新近纪时期则在祁连造山带与昆仑造山带之间形成双侧前陆盆地，第四纪属挤压坳陷盆地。