LITHOLOGY INTERPRETATION BASED ON WELL LOG DATA ANALYSIS IN “JS” FIELD

T. W. Sari, S. Sujito
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Abstract

Reservoir lithology types in a prospect zone of hydrocarbon can be known through well log data analysis, both qualitatively and quantitatively. Lithology interpretation based on qualitatively well log data analysis, has been successfully carried out by K-1 and K-3 well log data on JS Field, West Natuna basin, Riau Islands.Main focus of the research is types of lithology indicated by response the petrophysical well data log of Lower-Middle Miocene Arang Formation. Arang Formation was deposited immediately on top Barat formation and depositional environment in this formation is transitional marine - marine. Petrophysics log shows well data are log gamma ray, resistivity, neutron porosity, density, and sonic. The limitation of study are on four types lithology, they are coal, sand, sally sand, and shale. Lithology on well K-1 dominate by shale, there is thin intersection between sand and coal. The well of K-1 have sand thickest around six meter. While on well K-3 Petrophysics log data shows thin intersection between coal, sand, shaly sand, and dominated by shale. The thickest Sand have thickness 29 meter, and thicker than on K-1 well. The result in this study, the formation dominated by types of lithology “shale”.
基于测井资料分析的“js”油田岩性解释
通过测井资料的定性和定量分析,可以了解油气远景区储层岩性类型。利用廖内群岛西纳土纳盆地JS油田的K-1和K-3测井资料,成功地进行了基于定性测井资料分析的岩性解释。研究的重点是响应中-中新统阿朗组岩石物理测井资料所指示的岩性类型。Arang组直接沉积于Barat组之上,该组沉积环境为过渡性海相-海相。岩石物理测井数据包括测井伽马、电阻率、中子孔隙度、密度和声波。研究局限于煤、砂、砂、页岩四种岩性类型。K-1井岩性以页岩为主,砂煤相交较薄。K-1井的沙子厚度在6米左右。而K-3井的岩石物理测井数据显示,煤、砂、泥质砂之间有很薄的交集,且以页岩为主。最厚砂厚29米,比K-1井更厚。研究结果表明,该地层岩性类型以“页岩”为主。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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