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印尼K区块中下侏罗统储层流动单元研究
引用本文:宋俊朋,张立强.印尼K区块中下侏罗统储层流动单元研究[J].甘肃科学学报,2016(6):23-30.
作者姓名:宋俊朋  张立强
作者单位:中国石油大学 华东 地球科学与技术学院,山东 青岛,266580
摘    要:以印尼K区块R组海相砂岩储层为研究对象,结合国内外流动单元研究现状,分析了岩心、测井和储层物性等,对R组储层流动单元的划分、特征、控制因素等进行了研究。分析结果表明:采用FZI法可将印尼K区块R组划分为7种流动单元类型,不同流动单元物性差别较大,其中HFU-6和HFU-7是研究区最有利流动单元类型。通过对工区数据分析可知,工区流动单元受沉积环境和成岩作用的影响较大,在区域上,工区从南向北有利流动单元分布厚度逐渐增大。

关 键 词:R组  流动单元  FZI  储层物性  沉积环境

Research on Flow Unit of Middle and Lower Jurassic Reservoir in Indonesia K Block
Abstract:Take the marine sandstone reservoir of R group in Indonesia K Block,combine with the foreign and domestic research status about flow unit and based on the analysis of information such as core,logging and reservoir physical property to research on the division,characteristic and controlling factor of flow unit of R reservoir.The analysis results show that the R group in Indonesia K Block can be divided into 7 flow unit types according to FZI method,physical property difference between different flow units are large and among them,the HFU-6 and HFU-7 are the most favorable flow unit types in the research area.Ac-cording to the data analysis of working area,the sedimentary environment and diagenesis have large influ-ences on the flow unit in working area and in terms of area,the distribution thickness of favorable flow u-nit within the working area is gradually increasing from south to north.
Keywords:R group  Flow unit  FZI  Reservoir physical property  Sedimentary environment
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