次级断层的英文

• second-order fault
• secondary order fault

• "次级"英文翻译    secondary
• "断层"英文翻译    fault; slip; slicle; fractur ...
• "次级断块" 英文翻译 :    secondary fault block
• "二级断层带" 英文翻译 :    second-order fault zone
• "次级同向断层" 英文翻译 :    homothetic faults
• "次级相向断层" 英文翻译 :    synthetic faults
• "次级" 英文翻译 :    secondary
• "初级断路器" 英文翻译 :    primary cutout
• "三级断路器" 英文翻译 :    three-pole breaker
• "两级断开系统" 英文翻译 :    two-stage cut system
• "断层" 英文翻译 :    fault; slip; slicle; fracture; dislocation 倾向断层 dip fault; 走向断层 strike fault
• "梯级断链安全装置" 英文翻译 :    stechain safety device
• "次级,二级" 英文翻译 :    sec secondary
• "次级；辅助" 英文翻译 :    secondary
• "次级板" 英文翻译 :    secondary plate
• "次级表" 英文翻译 :    secondary table
• "次级波" 英文翻译 :    secondary wave
• "次级仓" 英文翻译 :    secondary stockroom
• "次级层" 英文翻译 :    sub-layer
• "次级场" 英文翻译 :    secondary field
• "次级船" 英文翻译 :    substandard ship
• "次级蛋" 英文翻译 :    substandard eggs
• "次级的" 英文翻译 :    antepenultimate; inferior; secondary; subordinated; ungraded
• "次级端" 英文翻译 :    out secondary
• "次级港" 英文翻译 :    secondary port

• According to the geological features of dongying movement in bohai bay basin and the research results of the former , this paper analyzed the potential geodynamic origins of dongying movement
  形成了众多小规模次级断层、全区整体抬升并遭受剥蚀，局部发育反转构造。
• The fault zone passes through the offshore between the changdong islands and the dazhudao island , and consists of a group of nw trending faults , which are dominated by normal and reverse slips with strike - slip component
  该断裂带由一系列北西走向的次级断层组成，主体在长岛至大竹岛之间的海域，多数断层以正断兼有走滑运动为主，部分断层具有逆冲运动性质。
• Due to the multi - period tectonic movement and evolution of mechanical mechanism , syndeposition structures occur extensively in jiyang sag , the base of the sag subsided alternatively during the fault depression , which resulted in sinking of top bending and complicated block structure accordingly , reconstructed the syndeposition intensively , and produced the special structural landscape in combination with all levels of faults and sedimentary formations within it
  摘要济阳坳陷由于受到多期构造运动的影响，在前第三系古地形高点背景上广泛发育同沉积背斜构造，然而由于坳陷在断陷期基底滚动式沉降，造成挠曲顶部的塌陷，形成复杂的块断结构，使本区同沉积构造发生强烈改造，往往与各次级断层或沉积地层相复合，表现出独特的构造景观。