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连井的英文

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"连井"怎么读用"连井"造句

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  • well tie

例句与用法

  • Even the well itself was empty .
    甚至连井也是空的。
  • Basing on the analysis and correlation of the7 wells , 8 seismic sequence boundaries are obtained by logging - seismic correlation , based on seismogram synthesis . more over , they can be traced in the studying region . the synchronic sequence stratigraphic framework is established finally
    在单井分析和连井对比的基础上,通过合成记录标定、地震层序的分析,识别出8个三级层序界面,而且完成了全区的主干剖面解释,建立了井震统一的等时层序地层格架。
  • Under the guidance of new principles and methods of modern sedimentology , detrital petrography , reservoir geology , diagenesis , this thesis has carried out detailed study on paleogene formation correlation , sedimentary environment , characteristics of sedimentary facies and diagenesis of the eastern kuche depression , tarim basin , dina area being taken as the main target of the study . based on the core , geology logging , log and seismic data from 9 typical wells , combined with the data of the adjoining area , the dominant sedimentary types of the study area have been recognized and illustrated , such as fan - delta , lacus and normal delta . in terms of the analysis on the sedimentary facies of typical and connecting wells in different areas and facies belt , together with the paleogene tectonic evolution characteristics of foreland basin , the distribution and evolution of the sedimentary facies of the study area have been clearly discovered both vertically and laterally
    通过对该区9口井的岩芯、录井、测井、地震资料及邻区资料的分析,识别并阐述了库车坳陷东部下第三系的几种主要的沉积相类型,如扇三角洲相、湖泊相和正常三角洲相;通过对不同地区、不同相带典型井及连井的沉积相分析,结合前陆盆地在下第三系的构造演化特点,弄清了迪那地区下第三系沉积相的纵横相发育展布和演化规律,并建立了沉积相模式;同时,初步开展了成岩作用、储层孔隙演化和储层发育模式的研究工作,科学合理地解释了现今迪那地区下第三系储产层主要发育在粉砂岩中的特殊现象,首次建立了下第三系储层的发育演化模式,为库车坳陷东部地区进一步寻找下第三系大储量、高产油气藏和有利的勘探区块提供科学的、可靠的和最直接的地质依据。
  • From connecting - well profiles that reflect filling characteristic of basin , combining with comprehensive analysis of seismic stratigraphic framework , the sequence stratigraphic framework of tertiary was established in hong - shi area and the distribution of sedimentary systems in time and space was deeply discussed
    通过能揭示区内第三系沉积充填特征的连井剖面,结合地震层序地层格架的综合分析,建立起了红狮地区第三系的层序地层格架,探讨了沉积层序的时空分布规律。
  • Through the analysis of petrology characteristics and individual well section of sedimentary facies of five core holes , direction of sedimentary source area , the depositional framework and main facies types and its features of penglaizhen formation , baimamiao - songhua area are elaborated on the basis of sedimentary backgroud of region . from this above , in view of the study of the correlation of 3 cross sections of sedimentary facies , it is pointed out that distribution regularities of sedimentary facies and possible places of distribution of sand bodies of iii , iv member of penglaizhen formation are vertically and laterally developed in baimamiao - songhua area . by the analysis and contrast of seven plans of sedimentary facies and nine isopach maps of sandstone , the planar characteristics of distribution of sedimentary facies are summarized , meanwile , macroscopic distribution regularities of sand bodies is studied in iii , iv member , penglaizhen formation of baimamiao - songhua area
    通过5口取心井的岩石学特征、单井剖面相分析,结合区域沉积背景,阐述了研究区蓬莱镇组的物源方向、沉积格局、主要沉积相类型及其特征;在此基础上,通过3条连井剖面的沉积相对比研究,揭示了研究区蓬段、蓬段纵向与横向上沉积相的分布规律及砂体的大体分布位置;通过7张沉积相平面图、 9张砂岩等厚图的分析对比,总结了蓬段、蓬段沉积相的平面分布特征,宏观上研究了蓬段、蓬段的砂体展布规律。
  • Under the guidance of new principles and methods of sedimentology and reservoir sedimentology , this thesis takes jialingjiang formation in qianwei area as the main object of study . the petrology characteristics and sedimentary facies of nine basic wells have been studied exhaustively , from which it is deducted the depositional framework , and main types and characteristics of sedimentary facies in jialingjiang formation . then four types of sedimentary facies are recognized and their facies models are established
    本论文以现代沉积学与储层沉积学的新理论、新观点、新方法为指导,以犍为地区嘉陵江组为重点研究对象,通过9口基干井的单井岩石学特征、沉积相的分析,阐述了犍为地区嘉陵江组的沉积格局以及主要的沉积相类型与特征,识别出了四种不同类型的亚相,并分别建立了沉积相模式;在单井沉积相分析的基础上,通过三条连井剖面沉积相的对比研究,阐明了犍为地区嘉陵江组沉积相的纵向与横向发育规律。
  • ( 5 ) based on the integrated sequence stratigraphy analysis of typical wells section and many well - to - well section , the control of hinge fault is confirmed . system tracts of downfaulted block perfectly develop , from lower position to higher position , upfaulted block ( west - north region of the gentle slop ) is in turn pgc , tst , hst , overlapping in sb
    ( 5 )通过典型井剖面及众多连井剖面的层序地层分析,证实枢纽断层的控制作用,断层下降盘各体系域发育完整,而其上升盘(西北斜坡区)由低处向高处,依次是pgc 、 tst 、 hst超复于sb之上。
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