ISSN 1673-8217 CN 41-1388/TE
主管:中国石油化工集团有限公司 主办:中国石油化工股份有限公司河南油田分公司
全永旺, 姚光庆, 董晓霞, 周锋德, 刘斌, 黄郑. 2007: 焉耆盆地宝北区块厚层砂体夹层成因类型及结构模式. 石油地质与工程, 21(02): 9-12+7.
引用本文: 全永旺, 姚光庆, 董晓霞, 周锋德, 刘斌, 黄郑. 2007: 焉耆盆地宝北区块厚层砂体夹层成因类型及结构模式. 石油地质与工程, 21(02): 9-12+7.
2007: Genetic type and structure pattern of the interlayer inside thick sandbody of Baobei block in Yanqi basin. Petroleum Geology and Engineering, 21(02): 9-12+7.
Citation: 2007: Genetic type and structure pattern of the interlayer inside thick sandbody of Baobei block in Yanqi basin. Petroleum Geology and Engineering, 21(02): 9-12+7.

焉耆盆地宝北区块厚层砂体夹层成因类型及结构模式

Genetic type and structure pattern of the interlayer inside thick sandbody of Baobei block in Yanqi basin

  • 摘要: 宝浪油田宝北区块主力油层属侏罗系三工河组辫状河沉积砂砾岩体,夹层类型及结构模式严重影响油田注水开发效果。在岩心、测井等资料分析的基础上,识别出宝北区块沉积和成岩成因的4种夹层类型:泥岩夹层、煤质夹层、致密夹层、钙质夹层,并从单层间和单层砂体内2个层次对夹层结构和展布规律进行了详细研究,旨在为油田生产开发提供地质依据。从稳定性角度,可分为稳定夹层、较稳定夹层、欠稳定夹层和不稳定夹层4种结构类型夹层,并结合沉积微相对夹层分布进行总结:单层问夹层平面上一般出现在河道间湾或废弃河道的顶部及河道末端部位,单层砂体内夹层在平面上主要出现在辫状分流河道内,其次是河道侧缘及分支间湾,河道间出现较少。

     

    Abstract: Major reservoir of Baobei block in Baolang oilfield be- longs to Glutenite units in braided river of Sangonghe for- mation of Jurassic.The types and structure pattern of in- terlayer greatly affect the water-flooding development results.Based on the analysis of drilling core and well log,four types of interlayer have been identified:sand- stone interlayer,coaly interlayer,compact interlayer and calcareous interlayer.The study on interlayer structure and its distribution on two levels-between monolayers and inside monolayer provide geological guidance for oil- field development.From the angle of stability,four types are classified:stable,relatively stable,under stable and instable. With the combination of sedimentary micro-facies, the distribution patterns are summarized:interlayer be- tween monolayers commonly occurs at channel bay or the top of abandoned channel,or the end of channel;the in- terlayer inside monolayer sand body,mainly occurs inside braided distributary channel,secondly occurs at channel side and interdistributary bay,occasionally occurs at channel.

     

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