首页> 外文会议>Annual Indonesian Petroleum Association convention and exhibition >RESERVOIR GEOMETRY IDENTIFICATION OF TIDE DOMINATED ESTUARINE ENVIRONMENT DEPOSITS AND ITS IMPLICATION TO RESERVOIR QUALITIES: CASE STUDY WITHIN THE UPPER SAND OF BEKASAP FORMATION, GADANG FIELD,CENTRAL SUMATRA BASIN, INDONESIA
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RESERVOIR GEOMETRY IDENTIFICATION OF TIDE DOMINATED ESTUARINE ENVIRONMENT DEPOSITS AND ITS IMPLICATION TO RESERVOIR QUALITIES: CASE STUDY WITHIN THE UPPER SAND OF BEKASAP FORMATION, GADANG FIELD,CENTRAL SUMATRA BASIN, INDONESIA

机译:潮汐河口环境沉积物的储层几何学识别及其对储层质量的影响:以印度尼西亚中部苏门答腊盆地加当油田贝卡萨布组上砂为例

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Gadang Field is one of hydrocarbon field which located in Central Sumatra Basin. The production in sand reservoir of the upper part of Bekasap Formation in this field identified is still not optimum. Because of this term, need a geological understanding of reservoir body for future potential development by generate a redefinition of reservoir to understand the condition of reservoir, such as geometry, distribution, and quality of reservoir for proper plan/method in the future development.The methods that are being used in this study are depositional environment interpretation by core data in the sand body of the upper part of Bekasap Formation; understanding geometry and distribution of reservoir by analysis from gross facies unit map and net sand unit map; and characteristics of reservoir determination by using vshale and effective porosity. This study is using 83.5 feet core data from 2 wells and well log data from 16 wells.Core detail description was end up with two facies associations identified, named cross-bedded - coarse sandstones facies association (estuarine channel) and flaser-laminated - fine sandstones facies association (tidal sand flat/sand bar). This two facies associations were interpreted as tide dominated estuarine environment deposit consider with estuarine depositional environment model developed by Dalrymple (1992). By geometry analysis, there are two different geometry of reservoir from this one reservoir zone, such as "channel" sand body (estuarine channel) and "tidal sand flat/sand bar" sand body (tidal sand flat/sand bar), which influenced by mechanism of depositional environment from each facies. Reservoir characteristics analysis based on vshale and effective porosity, indicate that the sand body which deposited in estuarine channel relatively has a better reservoir quality than the sand body which deposited in tidal sand fLat/sand bar.
机译:加当油田是苏门答腊盆地中部的油气田之一。在确定的该油田中,Bekasap组上部砂储层的产量仍然不是最佳的。由于这个术语,需要通过重新定义储层以了解储层的状况(例如储层的几何形状,分布和质量),以便在将来的开发中制定适当的计划/方法,从而对储层主体进行地质了解,以便将来进行潜在的开发。 本研究中使用的方法是通过Bekasap组上部砂体中的岩心数据解释沉积环境。通过总相单元图和净砂单元图的分析,了解储层的几何形状和分布;利用页岩和有效孔隙度确定储层特征和特征。这项研究使用了来自2口井的83.5英尺岩心数据和来自16口井的测井数据。 最终,对核心细节的描述是确定了两个相的组合,即交叉层-粗砂岩相协会(河口河道)和层状薄片-精细砂岩相协会(潮沙平面/沙洲)。 Dalrymple(1992)开发的河口沉积环境模型将这两个相联系解释为潮汐为主的河口环境沉积物。通过几何分析,这一储层带有两种不同的储层几何形状,例如“河道”砂体(河口河道)和“潮沙扁/沙洲”砂体(潮沙/沙洲),这对储层产生了影响。通过每个相的沉积环境机制。基于页岩和有效孔隙度的储层特征分析表明,沉积在河口河道中的砂体比沉积在潮滩/沙洲中的砂体具有更好的储层质量。

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