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投点的英文

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"投点"怎么读用"投点"造句

英文翻译手机手机版

  • cultellation

例句与用法

  • Dobson ! get some tear - gas in that house
    都布森!投点催泪瓦斯进去!
  • At level 5 , the exploration sheet is available if you wish to spend some points in it
    5级的时候,探索单(技能分支)可以被投点
  • Thirdly , large scope random - cast point methods and partition interval methods are addressed
    三是提出了随机投点和分割区间方法。
  • We need a body down low who can hassle , rebound and score a bit
    我们需要一个能冲向内线,能玩命打球,能抢蓝扳的,能投点蓝的小伙。
  • Point of no return
    不?投点
  • Nothing like getting hung up and repeatedly missing your target to provide the motivation
    一而再,再而三的挂住障碍物和错偏目标抛投点,就是他们转变的动机。
  • Resurvey the column axis and elevation line , and mark out the column form line , 1 : 2 cement mortar will be used to leveling at the column bottom . “ 井 ” shape rack will be set around each column , and mark elevation control line on it
    将柱轴线、标高线复测投点,弹出柱支模线,将柱脚支模处用1 : 2水泥砂浆找平,每根柱周围搭设井字架,在井字架上抄测标高控制线。
  • On the basis of the analysis of the characteristics of deep well relation measurement and through the on - site test and theoretical analysis , the methods and technical measures of the throwing - to - point , the orientation and the high - depth positioning in deep - well relation measurement are studied
    在分析深井联系测量特点的基础上,通过现场试验和理论分析,研究了深井联系测量的投点、定向、导入高程的方法及技术措施。
  • We find that the petrology characteristic of all the samples have no characteristic of meteoric water such as geopetal structure , infiltrative sand , ( uniform cement and gravitational cement on base of the research of the dolomite in the regions . on the dot diagram of combination of mgco3 ( mol % ) and sr , the dot are all close to the line of seawater whether they are microlite - crystalline penecontemporaneous dolostone or diagenetic dolostone of various crystals . the 87sr / 86sr value of dolostone or matrix is less than the one of sparry calcite in cave or vein , and close to the value of seawater
    通过本区白云岩的研究发现:已有的白云岩样品的岩石学特征没有显示出如示底构造、渗滤沙、新月型胶结物和重力胶结物等大气淡水作用的特征;在白云石mgco _ 3mol百分数和白云石sr含量的投点图中,无论是准同生成因的泥?微晶白云岩,还是粉?细晶(或中晶,或细晶以上的不等晶)的成岩白云岩,均投在海水线的附近;白云岩(或基质)的~ ( 87 ) sr / ~ ( 86 ) sr比值显著低于与孔洞或脉中充填的亮晶方解石,且与海水值十分接近, ~ ( 13 ) c和~ ( 18 ) o值显著高于孔洞或脉中充填的亮晶方解石,也偏向于海水值; mn含量则显著低于孔洞或脉中充填的亮晶方解石。
  • According to the sr - nd isotopic characteristics of peridotite xenoliths and their host basalts , it indicates that xenoliths in hannuoba , puning area may represent source area of the host basalt because of the xenoliths and host rocks being in the same plot ; however , the xenoliths is not directly related to their host rocks of the others area for the xenoliths plot out of the range of their host basaltic rocks . thermal dynamics calculation shows that the peridotite xenoliths are formed in the condition of pressure of 9 . 45 - 25kb and temperature of 945 - 1281
    橄榄岩包体及其寄主玄武岩的sr - nd同位素研究表明,汉诺坝与普宁地区部分包体样品投点落在其寄主玄武岩nd和sr同位素的分布范围内,表明橄榄岩包体代表了寄主玄武岩的源区,而其它大部分地区的包体其寄主玄武岩范围之外,表明寄主玄武岩和橄榄岩包体无成因联系,橄榄岩包体只是偶然包体。
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