井剖面的英文

• well profile

• "井"英文翻译    well
• "剖面"英文翻译    bisect; section; profile
• "钻井剖面" 英文翻译 :    drill log; drill record; drilllog; well log; welllog
• "钻井剖面图" 英文翻译 :    graphic well log; graphicwelllog
• "电测钻井剖面" 英文翻译 :    electric well log
• "井剖面；井身结构" 英文翻译 :    well profile
• "生产测井剖面" 英文翻译 :    productoin-log profile
• "示踪测井剖面" 英文翻译 :    tracerlog profile
• "中子测井剖面" 英文翻译 :    gamma neutron log
• "柱状钻井剖面" 英文翻译 :    strilog
• "伽马测井剖面" 英文翻译 :    gamma log; gammalog
• "丛式井剖面设计" 英文翻译 :    multi-well profile planning
• "定向井剖面接近法" 英文翻译 :    directional well profile approximation
• "合成地震测井剖面" 英文翻译 :    seislog section
• "伽马 中子测井剖面" 英文翻译 :    gamma neutron log
• "伽马中子测井剖面" 英文翻译 :    gammaneutronlog
• "a-a剖面" 英文翻译 :    a a section; a-a section
• "剖面" 英文翻译 :    [地质学] bisect; section; profile 横剖面 cross section; 纵剖面 longitudinal section; 剖面符号 [图] section symbols; 剖面图 [电磁] sectional view; profile; bisect; profile chart; sectional drawing; section; 剖面线 hatch
• "半剖面" 英文翻译 :    semi-section
• "薄剖面" 英文翻译 :    thin section
• "波剖面" 英文翻译 :    wave profile
• "长剖面" 英文翻译 :    long-range profile
• "大剖面" 英文翻译 :    heavy gauge
• "陡剖面" 英文翻译 :    cliff section
• "断面，剖面" 英文翻译 :    profile

• It is indicated that cap layers classifying and lithological distinguishing in single well profile can be reached through well - logging facies analysis
  研究认为，从测井相分析的角度可以解决单井剖面地层中盖层划分与岩性识别的问题。
• When basement rock rupture pass through the well cross section , the fracture belts can be identified with some evidences , for example , the compensate neutron increasing and the stratum density diminishing synchronization , the dual - laterolog resistance diminishing greatly and the positive difference between the deep laterolog resistance and the shallow laterolog resistance appearing . when the compensate neutron increase , the stratum density diminishing and the dual - laterolog resistance value diminishing slightly , the fracture belts can be confirmed with the intrusive vein at high frequency in well cross section
  当有基岩断裂在井削面上通过时，若补偿中子增大与地层密度变小同步发生，双侧向测井电阻率有明显变低并有正差异出现，则可以判别为裂缝发育带；当补偿中子增大，地层密度变小及双侧向幅度变小都不太明显时，则可以利用井剖面中频繁出现的侵入岩脉来确定裂缝发育段。
• 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。