俯冲的的英文

• diving

• "俯冲"英文翻译    dive; downthrust; nose dive; ...
• "的"英文翻译    4次方是 The fourth power of 2 i ...
• "改出俯冲的动作" 英文翻译 :    pullout maneuver
• "进入俯冲的动作" 英文翻译 :    push-down-over maneuver
• "带滚转改出俯冲的动作" 英文翻译 :    rolling pullout maneuver
• "俯冲" 英文翻译 :    1.(飞机以高速度和大角度向下飞) dive; downthrust; nose dive; pitchdown; pique2.[地质学] (俯冲带) subduction 飞机笔直地俯冲下降, 然后又升起。 the plane dived sharply and then rose again
• "反冲的" 英文翻译 :    bucking; reactive
• "横冲的" 英文翻译 :    transcurrent
• "缓冲的" 英文翻译 :    buffered; buffering; sprung
• "急冲的" 英文翻译 :    intermittent
• "脉冲的" 英文翻译 :    pulsate; pulsing
• "猛冲的" 英文翻译 :    driving; gadarene; precipitant; precipitate
• "【火箭】俯冲。" 英文翻译 :    pitch-down
• "俯冲带" 英文翻译 :    subduction belt; subduction zone; subductionzone; underthrust zone, underthrust belt
• "俯冲机" 英文翻译 :    diver
• "俯冲角" 英文翻译 :    dive angle; diving angle
• "俯冲力" 英文翻译 :    underthrust
• "俯冲体" 英文翻译 :    underthrust mass
• "急俯冲" 英文翻译 :    nose dive
• "假俯冲" 英文翻译 :    dummy dive
• "正俯冲" 英文翻译 :    upright dive
• "多脉冲的" 英文翻译 :    multipulse
• "发射脉冲的" 英文翻译 :    exomomental; exomonental
• "过冲的界限" 英文翻译 :    bound on overshoot
• "后沿脉冲的" 英文翻译 :    back edge

• A little , but the rush was worth it
  一点点，但是俯冲的时候（危险）真是很值得的。
• B : a little , but the rush was worth it
  一点点，但是俯冲的时候（危险）真是很值得的。
• Andall ofthat will need to be nose - down pitched
  那都是在俯冲的时候必须的
• Andall ofthat will need to be nose - down pitched
  那都是在俯冲的时候必须的
• Ages of generation and subduction of shiquan river ophiolite : restriction from shrimp zircon dating
  测年对狮泉河蛇绿岩形成和俯冲的时间约束
• The helicopter is allowed to fall the same distance that it climbed at the beginning of the maneuver before pulling the helicopter back to straight and level flight
  待直升机垂直俯冲的距离与垂直爬升的距离相同时，拉起机头恢复成水平直线飞行。
• The giant eagle swooping over the billows ? when drawing an eagle , we have to capture its stately posture of fierceness and valor over rolling billows as its background
  巨鹰击浪图：画鹰一定要将其勇猛有力的雄姿画出来，背景配上澎湃的浪潮，藉鹰向下俯冲的姿态，让整个画面形成强而有力的动态美。
• The result of geodetic inversion shows that india block moves at rates of 20 . 4 millimeters per year with respect to the stable eurasia , consistent with the result comes from geology . this indicates that the rate india block moves towards eurasia is stable
  这与从地质推断的过去2 3百万年期间内，印度板块向欧亚大陆俯冲平均为18mm / y的速率大致相同，表明在较长时间范围内，印度板块向欧亚大陆俯冲的速率是稳定的。
• Chagan sag is a secondary tectonic unit in chagandelesu depression , northeastern yingen - eji ' naqi basin , and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate , with the character of erogenic belt . in working area and its adjacent area , the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly , intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase
  查干凹陷属于银根?额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元，其盆地基底为古生代时期华北板块、哈萨克斯坦板块和塔里木板块交接部位形成的陆缘或岛弧褶皱带，具有古生代造山带的性质。研究区及邻区印支期侵入岩形成于造山带强烈挤压陆内俯冲的构造环境；燕山早期侵入岩形成于由挤压转向拉伸、造山带的增厚陆壳开始发生伸展垮塌的构造环境；早白垩世火山岩形成于造山期后进一步发生伸展垮塌的区域构造环境。
• The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep . under the background of indian plate subducting under asia - europe plate , bachu forebulge was greatly affected by the development of southwest depression and awati depression . almost all of its structure reversed , and as a result of it , both of its south and north boundary migrated . according to its evolution history and its feature , the authors tentatively use both - side migration model to interpret the evolution of compound forebulge . since triassic , almost all the spheres above lithosphere synchronously became flexure . because transpressional stress field became increasingly strong , bachu forebulge continued uplifting and big faults formed . then , bachu uplift , as a whole , slipped upward along those big faults and showed migrating toward thrust zone in plane . in tectonic tranquility , the lithosphere bounded back and in consequence of it , bachu uplift slipped down and showed migration toward craton , at that moment negative inversion structures developed . while the forebulge migrated toward its south and north foredeep , it was very possible that locally extensional stress appeared in the forebulge
  在印度板块向欧亚板块俯冲的大背景下，巴楚前缘断隆受西南坳陷和阿瓦提凹陷的影响，新生代时构造体制发生反转，边界向南北迁移。根据其发育过程特征，作者用复合前缘隆起两端迁移模式对复合前缘隆起独特的构造发育史进行了解释：即三叠纪以来岩石圈各圈层同步挠曲变形。随着挤压应力场的增大，巴楚隆起在挠曲基础上不断抬升，形成几条大型断裂带。

• 俯冲的的法语：sous-charrié