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分带     
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  zoning
     ⑹Element zoning for 30 elements is: Mn Ag 1 Pb 1 Cd Zn Sn Cu Au Hg As Bi W Co Sb Mo Y Ni V Nb Sr Cr La Sc Ti Yb Be Ag 2 Pb 2 Ga B Ba.
     30种元素的分带序列为 :Mn Ag1 Pb1 Cd Zn Sn Cu Au Hg As Bi W Co Sb Mo Y Ni V Nb Sr Cr La Sc Ti Yb Be Ag2 Pb2 Ga B Ba。
短句来源
     SOME MINERAL EQUILIBRIA IN THE SYSTEM K_2O-Al_2O_3-SiO_2-H_2O-F_2O_(-1) AND THEIR APPLICATION TO ALTERATION ZONING IN PORPHYRY Mo,Sn DEPOSITS
     K_2O-Al_2O_3-SiO_2-H_2O-F_2O_(-1)体系中某些矿物的平衡关系及其对斑岩Mo、Sn矿床蚀变分带的应用
短句来源
     The axial zoning sequence of primary halos is As-Sb-Ag-Bi-Pb-Hg-Au-Zn-Cu.
     原生晕轴向分带序列为As-Sb-Ag-Bi-Pb-Hg-Au-Zn -Cu,横向分带序列为 ,矿体上部原生晕 :Au -Zn -Ag -Bi-As-Hg -Cu-Sb -Pb ;
短句来源
     Axial zoning sequence of the indicator elements is described as follows: As—Ag—Sb—Cu—Zn—Au—Pb—Ni—Co, on the basis of this, the following formulas for predicting buried depth of the ore body are established. H=38.790 As/Co+442.842 LnH=0.0923Ln[(As, Ag, Sb)/(Au, Co, Ni)]
     指示元素的轴向分带序列为:As—Ag—Sb—Cu—Zn—Au—Pb—Ni—Co,并以此建立了预测矿体埋藏深度关系式:H=38.790As/Co+442.842 LnH=0.0923Ln[(As.Ag.Sb)/(Au.Co.Ni)]+6.3116
短句来源
     Its indicator elements are Cu,Pb,Zn,Ag,Cd,Hg,As,Sb,Au,Ba,Sr and B.The sequence of axial zoning or vertical zoning(from top to bottom) is Zn-Hg-Pb-Ag-Cu 1-Ba-Sr-Sb-As-Cu 2, Ni,Co,Au.
     指示元素有Cu、Pb、Zn、Ag、Cd、Hg、As、Sb、Au、Ba、Sr、B等,原生异常的轴向分带序列(从上到下):Zn-Hg-Pb-Ag-Cu1-Ba-Sr-Sb-As-Cu2、Ni、Co、Au,具有明显多建造晕的特点。
短句来源
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  zonation
     the perpendicular zonation is Cu→Zn→Sn→Ag→Pb→Mo→In→Bi→As(from the lower to the upper).
     垂直分带序列(从下至上):Cu→Zn→Sn→Ag→Pb→Mo→In→Bi→As;
短句来源
     The deposit is characterized by vertical Mn(Fe)-Ag,Pb,Zn-Cu,Pb,Zn zonation.
     该矿床从上至下具Mn(Fe)-Ag,Pb,Zn-Cu,Pb,Zn的垂直分带规律。
短句来源
     The horizontal zonation of metallic element(from the inner to the outer) is Cu-Bi→Ag→Sn→Pb-Mn→Cd;
     金属元素水平分带(从内向外):Cu、Bi→Ag→Sn→Pb、Mn→Cd;
短句来源
     From far source to near source,with the mineralizing zonation of Au,Ag Au,Cu,Ag Cu,Au,Pb,Zn Cu(Mo,Au),the ore forming temperatures change from low to high; while the sulphide contents vary from poor to abundant.

     从远源至近源,成矿分带为Au、AgAu、Cu、AgCu、Au、Pb、ZnCu、(Mo、Au),成矿温度从低温至高温变化,硫化物从贫硫化物向富硫化物变化.
短句来源
     Geochemical mapping shows that some geochemical parameters, such as Sn, W, REE, Zr, Th, and Rb, exhibit a rough spatial zonation, with the most evolved samples located in the southeastern part of the pluton, suggesting that the most probable target area of rare-metal deposits may be in the southeastern area, i.e., between 116°8′E~116°10′E and 25°29′N~25°32′N.
     地球化学填图显示了元素在空间上的分带变化,指出与红山花岗岩有关的成矿作用最可能发生在岩体的东南端,即116°8′E~116°10′E和25°29′N~25°32′N的区域。
短句来源
更多       
  zoning caused
     i. e. (1) Zoning of mineralization types caused by the mechanical properties of ore-controlling fracture, (2) Pulsation zoning caused by the mineralization of multiple stages and, (3) Zoning caused by precipitation in the same mineralization stage.
     即:(1)受控矿断裂性质制约的矿化类型分类; (2)由多阶段矿化形成的脉动分带和,(3)由同一阶段矿化形成的沉淀分带.
短句来源
     Because of composition zoning caused by liquid crystal fractionation in magmatic chamber the evolutionary tendency of the volcanic rock series shows two large periodical variations from acidic rocks to medium acidic by alkalic rocks.
     由于岩浆在岩浆房中发生了液晶分异作用,导致成分分带,因而使火山岩系的演化趋势从酸性向中酸偏碱性过渡,呈现两大周期性变化。
短句来源
  zoning distribution
     The paper discusses the hydrothermal filling deposit of W-Bi-Mo quartz vein type and the vertical reverse zoning distribution of wolframite-bismuthinite- molybdenite mineral group .
     简要论述了典型热液裂隙充填钨—铋—钼石英脉矿床地质及其以黑钨矿—辉铋矿—辉钼矿为主的矿物组合纵向逆分带现象。
短句来源

 

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      zoning
    Zoning by Functions of Small-Scale Forest Ecosystems: A Case Study of Hui-Sun Forest Station in Taiwan Province, China
          
    Based on the methods of landscape ecology and ecological planning, this paper develops a zoning project of ecosystem functions suitable for various environments.
          
    The composition of the forest-forming species and zoning are less affected.
          
    Catagenetic alterations of sedimentary sequences from these regions are analyzed and the general scheme of catagenetic zoning in elision basins is proposed.
          
    Their differences in age, host environment, formation depth, vertical extent of ore deposition, and zoning are also outlined.
          
    更多          
      zonation
    Some mechanisms of mineralogical and geochemical differentiation, which contribute to the facies zonation, are revealed.
          
    A pronounced vertical zonation is revealed in the spatial succession of different macrobenthos communities.
          
    Original schemes of faunistic zonation of the North Pacific are given.
          
    Fractal features and morphological differences between periodic infiltration and diffusion metasomatic zonation
          
    The choice of reference soils should be made with due account for the provinces of the soil-geographical (or soil-ecological) zonation as territories characterized by similar environmental conditions and typical soil cover patterns.
          
    更多          
      zoning caused
    Oscillatory zoning caused by oscillating surface relaxations
          


    ~~

    对使用361炉后的鞍铜平炉炉顶镁铝砖进行了分带化学分析、硝酸铵溶液处理、X射线物相分析、岩相鉴定及气孔率、体积密度、真比重、第Ⅰ带的耐火度、低熔物出现温度和热膨胀等物理性质测定。 根据研究结果,对镁铝砖在使用过程中段带的形成、损毁过程和氧化铝的作用等问题提出了商榷意见。指出镁铝砖与镁铬砖具有不同的损毁过程。

    First of all, this paper deals primarily with the theory of affine transformation for

    木文首先用射影几何讨论了航摄象片纠正的仿射变换理论,说明象片与倾斜地平面图形的仿射投影,可直接构成透视射影对应.亦郎可将倾斜地平面的象片,直接通过象片纣正的仿射变换,一次纠正成水平象片.其投影中心只在平行纠正面的平面内移动.并推导出投影中心变化后的新坐标位置,以及航摄象片纠正的仿射变换纠正元素.其次,在纠正的仿射变换原理的应用及应用中的一些问题中,讨论了倾斜面(象片)纠正的地面倾角与纣正系数的选取、两次纠正、纠正对点问题、倾斜面分带纠正投影差改正公式、以及换带时附加额外偏心问题.并应用纣正的仿射变换原理,分析了大型纠正仪、小型纠正仪、光学投影器的偏心问题.最后通过实验,验证了上述理论的正确性.

    paoTbI o paHbIM MecTaM co cBoa (cMeHeHHoo B cebMo pa) MapTeHoBckoe № 1 Ha THbHckoM cTaeaBbHoM aBoe, bI BTbI opabI MaHeTo-HoeMHbIx kpe, paoTaBx oce 1835 aBok. o oHaM opaoB bI po-BeeHbI xMeck aHa, Mkpockoeckoe HaeHe ko-MexaHeckoecbITaHe. KpoMe Too, bI oToBeHbI MTaoHHbIe opabI, a TaKe cbITaHacTokocTb MTaoHHbIx opaoB opaoB HoBbIx pe poTB TeMepaTypHookoeaH p oBbIeHHbIx TeMepaTypax. PeybTaTbI cbITaH okaa, ToMaHeTo -HoeMHbIe kp oce cybI MoHo BbIeTb Ha Tp oHbI: eppo-oaTy, ckaTooaTy HeMeHeHHy oHy. B eppooaTo oHe epkaoBaaa...

    paoTbI o paHbIM MecTaM co cBoa (cMeHeHHoo B cebMo pa) MapTeHoBckoe № 1 Ha THbHckoM cTaeaBbHoM aBoe, bI BTbI opabI MaHeTo-HoeMHbIx kpe, paoTaBx oce 1835 aBok. o oHaM opaoB bI po-BeeHbI xMeck aHa, Mkpockoeckoe HaeHe ko-MexaHeckoecbITaHe. KpoMe Too, bI oToBeHbI MTaoHHbIe opabI, a TaKe cbITaHacTokocTb MTaoHHbIx opaoB opaoB HoBbIx pe poTB TeMepaTypHookoeaH p oBbIeHHbIx TeMepaTypax. PeybTaTbI cbITaH okaa, ToMaHeTo -HoeMHbIe kp oce cybI MoHo BbIeTb Ha Tp oHbI: eppo-oaTy, ckaTooaTy HeMeHeHHy oHy. B eppooaTo oHe epkaoBaaa cBbIBaeTc Mey coo, opay MoHoT epeHkypHo paoe oBepxHo-cT kpe, B He pacoaaTc aoHeHHbIe ckaTHo cBko opbI kaHabHoopMbI, HaoMHae "ecTy cTpykTypy". CkaTooaTa aa MeeT xapakTep-Hy cTpykTypy, HaoMHay "acabToBy MocToBy". ecb acTbI epkaaoTebHo pacoaaTc cpe HepepbIBHo ckaTHo MaccbI. AHay oy-eHHbIe aHHbIe bIo ycTaHoBeHo, To BHyTpeHHo pHo oTcoeH MaHeTo-HoeMHbIx kpe BeTc Hka MexaHecka poHocTb ckaTooaTon oHbIp BbIcokx TeMepaTypax, a BaHeM ycoBM oTcoeH x BTc koHcTpyk-TBHoe TepMeckoe HapeH.

    对天津钢厂1~#平炉第七届镁铝砖炉顶,在完成炉役(炉令1835炉次)之后,自不同部位取样,分带进行了化学分析、显微镜观察和物理-力学性质测定。也制备了部分模拟试样,试验了模拟试样及原砖样在高温下抵抗温度波动的能力。实验结果表明,使用后的镁铝砖可以分为三个带:铁氧富集带、硅酸盐富集带和未变带。铁氧富集带中的方镁石相接触在一起趋于一个整体,并且沿与作业面垂直的方向取向。方镁石相内分布着有硅酸盐存在的渠道状孔隙,而使这一带具有“蜂窝煤”状特征的结构。硅酸盐富集带则是孤立的方镁石颗粒分布在连续的硅酸盐基质内的形似“柏油路”的结构。通过对实验数据的综合分析,认为镁铝砖的硅酸盐富集带的高温强度低是其剥落损坏的内因,结构应力和热应力是其剥落损坏的重要条件。

     
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