Uncovering The Potential of Low Resistivity Reservoirs Through Integrated Analysis: A Case Study from The Talang Akar Formation in The South Sumatra Basin

Fiqya Fairuz Zaemi, Rian Cahya Rohmana, W. Atmoko
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Abstract

The study area is an oil and gas field that has a low resistivity reservoir zone in the Talang AkarFormation, South Sumatera Basin. The reservoir zone is composed of siltstone and sandstone that was depositedin a shallow to transitional marine environment. The aim of this study is to identify and determine the potential oflow resistivity reservoirs in the study formation. The data used in the study include well log, mud log, core data(porosity, permeability, petrography), formation water analysis, and biostratigraphy. The methodology includesqualitative analysis to determine reservoir potential zones (quick look interpretation) and the reason for low resistivityreservoirs, as well as quantitative analysis to calculate petrophysical parameters. The results of the quicklook analysis showed 77 low resistivity reservoir zones, but the petrophysical analysis identified 25 low resistivityreservoir zones as potential candidates for drill steam test (DST). Factors causing low resistivity reservoirs inthe study area include clay mineral content (kaolinite and illite), conductive minerals (pyrite and siderite), highsalinity formation water (10,000 ppm), very fine to medium sand grain size (0.063 - 0.5 mm) distribution ofclay minerals (laminated and dispersed clay), and thin laminates. The results of the petrophysical analysis showthat shale volume is less than 30%, porosity is greater than 14%, permeability is greater than 10 mD, and watersaturation is less than 70%.
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综合分析揭示低电阻率储层潜力——以南苏门答腊盆地Talang Akar组为例
研究区为南苏门答腊盆地塔朗阿卡组低阻储层油气田。储层由沉积于浅海至过渡海相环境的粉砂岩和砂岩组成。本研究的目的是识别和确定研究地层中潜在的低电阻率储层。研究中使用的数据包括测井、泥浆测井、岩心数据(孔隙度、渗透率、岩石学)、地层水分析和生物地层学。该方法包括定性分析以确定储层潜力区(快速解释)和储层低电阻率的原因,以及定量分析以计算岩石物理参数。快速分析结果显示了77个低电阻率储层,但岩石物理分析确定了25个低电阻率储层作为钻汽测试(DST)的潜在候选。在研究区形成低电阻率储层的因素包括粘土矿物含量(高岭石和伊利石)、导电矿物(黄铁矿和菱铁矿)、高矿化度地层水(10,000 ppm)、粘土矿物(层状和分散粘土)的极细至中等砂粒度(0.063 - 0.5 mm)分布以及薄层压层。岩石物理分析结果表明,页岩体积小于30%,孔隙度大于14%,渗透率大于10 mD,含水饱和度小于70%。
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