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后碰撞的英文

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"后碰撞"怎么读用"后碰撞"造句

英文翻译手机手机版

  • post-collision
  • rear collision (rear impact)
  • side collision

例句与用法

  • Frontal and rear vehicle collision test procedure
    车辆前碰撞和后碰撞的试验程序
  • Geochemistry of the carboniferous - permian post - collisional granitic rocks from tianshan
    二叠纪后碰撞花岗质岩石地球化学研究
  • Or , it may be described as : precollision granites syncollision granites postcollision granites
    亦可表述为:前碰撞花岗岩同碰撞花岗岩后碰撞花岗岩。
  • At this juncture , a private car driven by a 20 - year - old man reportedly rammed into the plb from behind
    据报此时该辆小巴被尾随的一辆私家车从后碰撞,而私家车是由一名二十岁的男子驾驶。
  • Geochronology research on the volcanic rock profile of the gazha cun group in the wuyii basin indicates that the 40ar - 39ar age of the post - collision volcanic rock is 12 - 14ma . and the granite that cut the volcanic rock is 10 . 84ma
    羊应乡火山岩样品中透长石及黑云母的~ ( 40 ) ar - ~ ( 39 ) ar定年结果确认该区存在后碰撞火山岩,其喷发年龄在11ma左右。
  • Integrated with other late paleoproterozoic granitoids within the central tectonic zone , it indicates that there was a tectonic transitional process from extension to compression during late paleroproterozoic in the southern segment of the central zone of ncc
    岩石学和地球化学研究表明王家会花岗岩属于后碰撞花岗岩,结合区域上古元古代地质特征,表明华北克拉通中部带南段古元古代晚期的花岗岩构成了与正常造山过程花岗岩浆演化相反的序列。
  • The results of combined internal mineral separates and whole - rock sm - nd isochron age for gabbro dikes from : luobusha , angren and xiubugabu in yarlung zangpo ophilite zone are 177ma , 166ma and 173ma respectively . the 4lar - 39ar step heating spectra of rikangba ophiolite suggest that its formation age is also isoma . it indicates that there was a stronger regionally inagmatism during middle - early jurassic , and the time of i75ma was the main period of the magmatic event of yarlung zangpo ophilite
    对邬郁盆地嘎扎村组火山岩剖面的年代学研究表明,该区后碰撞期火山岩的~ ( 40 ) ar - ~ ( 39 ) ar年龄为12 ? 14ma ,侵入其中的花岗岩脉的~ ( 40 ) ar - ~ ( 39 ) ar年龄为10 . 84ma ,与冈底斯西段前人研究资料对比,认为冈底斯带后碰撞火山岩时代有自西向东逐渐年轻的趋势。
  • Based on the study of geologic characteristics , such as mineralogic assembladge , structural and textural features of granite of guidong granitic massif , and by using petrochemical , trace - element and isotopic data , and some petrochemical , trace - element and isotopic diagrams widely applied to the identification of geo tectonic environments , authors recognize that guidong granitic massif was emplaced in post - orogenic collision environment
    摘要本文在研究贵东花岗岩岩体岩石矿物组合、结构构造等地质特徵的基础上,运用花岗岩的岩石化学、微量元素和同位素等分析数据,采用目前广泛应用的几种岩石化学图解、微量元素和同位素图解等方法,判别了贵东岩体形成的构造环境?造山带后碰撞型。
  • By having conducted 40ar - 39ar dating of 35 samples and sm - nd dating of 19 samples from the linzizhong volcanic rocks , the post - collision volcanic rocks and a granite dike and the yarlung zangpo ophilite , the dissertation provides significant new data and results for optimizing the time framework of tectonic - magmatic event s of this region . according to isotopic dating of 9 samples , 12 experiments survey in the main trunk profile , the eruption age of the linzizhong volcanic rock in the linzhou basin has been determined as 54 - 64ma
    本论文通过35个样品的~ ( 40 ) ar - ~ ( 39 ) ar及19个样品的sm - nd同位素测年,获得了关于俯冲?碰撞阶段形成的林子宗火山岩、后碰撞火山岩与花岗岩及雅鲁藏布蛇绿岩的同位素年龄数据,为完善研究区构造?岩浆事件的时间格架提供了新的资料与成果。
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