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三段的的英文

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"三段的"怎么读用"三段的"造句

英文翻译手机手机版

  • three-stage
  • three-step

例句与用法

  • Coffee sipped thrcugh the ice - cold cream . the last happy syrup . three seclions of feelings ccn dring unusual pleasanl surprise to you
    隔着冰凉的奶油啜饮着的咖啡,最后的甜蜜的糖浆,三段的感觉能带给您异常的惊喜。
  • The food may not be great , and the waitress may be surly , but those who stopped at red ? s will find that they are involved in the showdown of their life
    三段分别由卢克佩里、约翰萨维奇、埃瑞克罗伯斯与珍妮弗蒂莉主演,其中以第三段的表现最精彩。
  • The provisions in the first to third paragraphs apply also to anyone who has discovered and further developed a new plant variety or his successor in title
    以上第一段至第三段的条款亦适用于任何一发现并进一步发展出新的植物品种的个人或其名义上之继承人。
  • Subject to paragraph 23 below , where the vice - chancellor receives a complaint under these procedures , the vice - chancellor shall refer the complaint to the equal opportunity officer
    在符合第二十三段的规定下,校长在按本程序接获投诉后,会将投诉转介给平等机会主任。
  • However , sotx ti series racquets really have a lump of titanium in the built - in t - joint that applies three - stage method for combing racquets ' frame and shaft , updated from two - stage method
    由此,索牌钛系列球拍将块状的钛内置加上拍子的t型头区,使其发挥加固三段的作用,更新了拍框钛网眼或拍杆钛丝的加固二段的作用。
  • The paper analyzed sedimentary characteristics and depositional environment in t1f3 this region firstly , and on the grounds of establishing logical deposit pattern gave emphasis to make a study of distributing laws and spreading traits of the oolitic beach . because diagenesis is a vitally dominating factor that influenced oolitic beach reservoir nature in the region , the master diagenetic events of the reservoir in the lengthy geological history , as well as the influence to the pore abundance , was made a study of . the diagenetic stages and sequences were divided and the pore evolve pattern was established in the paper
    本论文首先分析了研究区飞三段的沉积特征与沉积环境,在合理建立沉积相模式的基础上重点研究了鲕粒滩(坝)的分布规律和空间展布特点;成岩作用是影响本区鲕滩储集性至关重要的控制因素,论文详细研究了储层在漫长地质历史过程中所经历的主要成岩事件及其对孔隙发育的影响,划分了成岩阶段与成岩演化次序,建立了孔隙演化模式并以建南构造为例进行了成岩相展布研究的尝试;最后还在鲕滩储层基本特征研究的基础上对飞三段储层进行综合评价与预测。
  • Directed by the advance theories of sequence stratigraphy , reservoir beds sedimentology , seismic stratigraphy and petro - geology , measured by exactitude seismic procession , analysis of seismic facies , analysis of single well lithfacies and sedimentary facies , study of macro and micro character of reservoir and diagenesis , this paper study comprehensively the stratigraphy sequence , the type and distributiong of sedimentary facies , reservoir properties , the diagenesis and the evolution of pores of the 2nd and 3rd parts of pingdiquan formation of permian in wucaiwan - shishugou region in jungan basin . we can optimum seek favourable target area and apply the study results on oil field production in order to solve the difficult questions . we mainly achieve several views as follows : l ) establish the sedimential sequence framework of permian formation in studying area and delimint the jiangjunmiao formation of middle dyas series as lowstand system tract , the lower of the second part to the third part of pingdiquan formation of middle dyas series as transgressive system tract , the upper of the second part to the first part of pingdiquan formation as highstand system tract
    以层序地层学、储层沉积学、地震地层学、石油地质学的先进理论为指导,以地震资料精细目标处理、地震相分析、单井岩相分析、沉积相分析、宏观和微观储层特征分析及成岩作用研究为手段,对准噶尔盆地东部五彩湾? ?石树沟地区二叠系平地泉组二、三段的地层层序、沉积相类型及展布、储层物性特征、成岩作用及孔隙演化进行综合研究,优选出有利勘探区带,并将研究结果应用到生产中,解决生产中的难题,主要取得了以下几点认识:建立了工区内二叠系沉积层序框架,把中二叠统将军庙组地层划为低水位体系域,中二叠统平地泉组二段下部三段地层为水进体系域,二段上部一段地层为高水位体系域。
  • The first power station of jinping mountain lies in the west section of the yanglongjiang river from santan to shoupagou gully , with a double - curved arch dam of 305 - meter height and a normal water storage of 1880metres . the exposed strata of the damsite are marbles and arenaceous rocks of triassic and solution fissures have been developed in the marbles of the left - bank ' s dam abutment , and they have become a stratum of strong leakage . as a result , it has been an important problem for the dam foundation to stop leakage
    锦屏一级电站位于西雅砻江的三滩至手爬沟河段,坝型为305米高双曲拱坝,正常蓄水位标高1880米。坝址区出露的地层为三叠系杂谷脑组二段大理岩和三叠系杂谷脑组三段的砂板岩。在勘探过程中,发现左岸坝肩大理岩体中的构造裂隙和溶蚀裂隙发育,且成为强渗透地层,为此坝基的防渗成为重要问题。
  • From studies of these characteristics of structures , palaeontology , drilling , well logging , seismic profile , salt chemistry and lacustrine sedimentary system , it is recognized that the new characteristics occur in of section pukou and in huaiyiri sag , and the huge thickness of salt rocks is formed by the crust salt materials upwelling along deep fracture in the form of hot bittern and entering lacustrine basin in this area
    通过该区构造、古生物、钻井、测井、地震、盐岩化学及湖盆内沉积体系等特征的研究,认为淮阴凹陷浦口组二段和三段的沉积构造有其特殊性,巨厚的盐岩层是壳深部盐类物质沿深大断裂上涌以热卤水形式进入湖盆的结果。
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