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  • facies type

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  • Based on the results of the study about the geological background in this area , this paper has discussed about the sedimentation facies marks for the fan delta in baimiao gas field , worked out a detailed proposal about the development of physical simulation experiment about the fan delta , and described in detail the general laws and major controlling factors governing the sedimentation processes of the fan delta . a detailed measurement was made about the experimental results , and a systematic comparison was made relative to the prototypic characteristics . based on the observation and description about the experimental processes and the analyses about the experimental results , this paper has given detailed
    在地质背景研究的基础上,对白庙气田扇三角洲沉积相标志进行了论述,在此基础上,制定了开展扇三角洲物理模拟实验的详细方案,详细描述了扇三角洲沉积过程的一般规律及主要控制因素;对实验结果进行详细的测量,并与原型特征进行了系统的对比,根据实验过程观察描述和实验结果分析,详细划分了白庙气田扇三角洲的岩石相类型及沉积微相;分22个砂层组完成了沉积微相尤其是扇三角洲上辫状河道展布规律的研究,分不同时期指出了22个砂层组砂体分布规律,为储层预测及该地区滚动勘探奠定了基础,这是本论文的重点内容之一。
  • We based on the analyse to main drill core of the area and adjacent , start with area stratum , set up microfacies type and identify characters of the area , make certain the types of facies and microfacies , and establish the mode of well logging microfacies . through synthetical contrast and analyze the layers and sand body of in pi formation of 316 wells , using well logging curves to partition and get 8 layers : pi1 - pi7 , in them p12 is thick formation , can be divided into p12a and p12b layers
    从区域地层、构造、沉积背景入手,以研究区和邻区的重点取芯井岩芯分析为基础,建立研究区沉积微相类型及识别特征,确定各小层亚相和微相类型,建立相应测井微相模式,依据研究区316口井的测井曲线资料将目的层pi组油层分为八个小层: p11 p17 ,其中p12层为厚油层,又可分p12a和p12b两个小层。
  • 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。
  • In the chronstratigraphic framework , the facies , the depositional system and the principle and range of reservoirs distribution are studied . the main depositional system is braided delta ? ub - lake fan . the coarse lithofacies which form braided delta depositional system is sub - water channel deposits ; the coarse lithofacies which form the sub - lake fan depositional system include turbidity channel deposits and bedded turbidity deposits
    在等时地层格架内,总结了各个中期旋回的沉积相类型、沉积体系和展布规律及范围,认为研究区在该时期以辫状三角洲?湖底扇沉积为主;构成辫状三角洲的粗碎屑相为水下分支河道;构成湖底扇的粗碎屑相包括:浊流水道相、层状浊积岩相。
  • 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。
  • It has been demonstrated that it is the microgel that guaranteed the homogeneous of the structure of the composite , the size and the morphology of the composite particles . the surface structure of the micro - particles can be adjusted by changing the preparing conditions . the composites may adopt hollow sphere structure , and the inner may lack of cds due to precipitation was started from the outer part of the microgels
    实验结果表明:高分子微凝胶的三维网络结构和所采用的制备方法确保了有机-无机复合材料复合的均匀性;微凝胶的模板作用使得复合材料呈球状结构,微球的大小决定于模板的尺寸;微球的微纳米结构可因微球的制备条件的不同(例如,改变连续相类型)而不同。
  • Based on the synthetic research of field outcrops , drilling section , well log and office compilation , combined with analyses of geological background , lithological association , sedimentary texture , sedimentary structure , geochemical and palaeobiological features , the researched area in the palaeozoic can be divided into deltas , braided deltas , lacus , barrier coast , continental shelf and carbonate platform etc . six kinds of sedimentary facies
    在野外露头、钻井剖面及测井曲线的综合研究和室内编图基础上,综合地质背景、岩性组合、沉积结构、沉积构造、地球化学及古生物学特征,研究区古生界被划分为三角洲、辫状河三角洲、湖泊、障壁海岸、陆棚及碳酸盐台地等6种沉积相类型
  • Finally , this paper analyzed reservoir characteristic of turbidite lithologic reservoir and the control iactors of oil and gas enrichment and high production and figure out that the major factors of influence and control reservoir are pressure , temperature , microfacies types , sand thickness , the action of fault , and the non - uniform feature of reserve by anatomizing typical reservoir
    最后,对浊积岩的储层敏感性反应和浊积岩岩性油藏的成藏特点及其富集高产的控制因素进行了讨论,认为砂体所处的压力和温度条件、沉积微相类型、砂层厚度、断层的活动及储层的非均质性等是其主要影响和控制因素。
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Last modified time:Thu, 14 Aug 2025 00:29:56 GMT

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