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:潮水型几何鉴定潮汐占据河口环境沉积及其对水库品质的含义:贝卡普地区上海案例研究,加兰省,中环苏门答腊盆地,印度尼西亚

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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:Gadang Field是位于苏门答腊盆地中部的碳氢化合物领域之一。鉴定在该领域的Bekasap地层上部的砂储存器中的生产仍然不是最佳的。由于这个术语,需要对水库身体的地质理解,以便通过生成储层的重新定义来了解水库的状况,例如用于未来发展的适当规划/方法的水库等地的水库。本研究中使用的方法是Bekasap形成的上部砂体中的核心数据的沉积环境解释;通过总体单元地图和净砂单元地图分析了解水库的几何和分布;使用谱系和有效孔隙度储层测定的特点。本研究采用来自2个井的83.5英尺的核心数据和来自16个井的井数数据。核心细节描述最终被识别的两个相关联,名为Cros-Bedded - 粗砂岩相结合(河口频道)和瓶层压 - 细砂岩相结合(潮汐砂扁平/砂杆)。这两个相关联被解释为潮德里林(1992)开发的河口沉积环境模型考虑潮汐主导的河口环境寄存。通过几何分析,从该水库区域有两种不同的储层几何形状,例如“通道”砂体(河道)和“潮汐砂平/砂杆”砂体(潮汐砂扁平/砂杆),影响通过每个相的沉积环境机制。基于vshale和有效孔隙率的储层特征分析表明,在河口通道中沉积的砂体相对具有比沉积在潮汐砂间/砂杆中的砂体更好的储层质量。

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