首页> 外文会议>Proceedings of The 38th IPA convention and exhibition-Strengthening Partnership to Enhance Indonesia’s Energy Resilience and Global Competitiveness >FLUID CONTACT ANALYSIS BASED ON FLUID REPLACEMENT MODELING ON DIRECT HYDROCARBON INDICATOR FEATURE IN THE MUNDU FORMATION, EAST JAVA BASIN
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FLUID CONTACT ANALYSIS BASED ON FLUID REPLACEMENT MODELING ON DIRECT HYDROCARBON INDICATOR FEATURE IN THE MUNDU FORMATION, EAST JAVA BASIN

机译:基于流体置换模型的东爪哇盆地蒙杜组直接油气指标特征的流体接触分析

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Seismic reflection anomaly in the form of bright flatrnspots have been observed and drilled in the MundurnFormation. This formation is a Pliocene bioclasticrnlimestone reservoir containing biogenic gas, whichrnis widely spread in the Madura Strait.rnMany gas discoveries in Mundu Formationrnconfirmed that the flat spot is associated with directrnhydrocarbon indicators (DHI). In well logs, thernDHI normally correlates with a single gas waterrncontact (GWC). An interesting finding here is thatrnmany wells encountered two fluid contacts; thernlowest mobile gas and the paleo-GWC.rnFluid replacement method was used to model thernphysical variations of the seismic trace response atrnthe bright spot level with varying gas saturations.rnWhen good seismic quality is available, this methodrncould identify the two fluid contacts and quantifyrngas saturation of the interval.rnThe model confirmed the zone between tworncontacts as residual gas zone. Observation on thernoccurrence of shallow gas and paleo-GWC suggestsrnthat shallow gas shows can be used as an indicatorrnof paleo-GWC existence.rnThe study concludes that the flat spot should be thernmain requirement for any drilling prospectsrntargeting gas in the Mundu Formation.rnThe characteristics of two fluid contacts can bernindicated by the shallow gas occurrence andrnidentified in the seismic trace. The ability torndistinguish two fluid contacts would reduce thernuncertainty in quantifying reserves.
机译:在Mundurn地层中观察到并以明亮的平斑形式出现了地震反射异常。该地层是上新世生物碎屑石灰石储层,含生物气,广泛分布于马杜拉海峡。蒙杜组的许多天然气发现证实了该平坦点与直接烃指示物(DHI)有关。在测井中,DHI通常与单个气体水接触(GWC)相关。有趣的发现是,许多井遇到了两个流体接触。最低的流动气体和古GWC。流体替换法被用来模拟在亮点水平具有变化的气体饱和度的地震迹线响应的物理变化。当可获得良好的地震质量时,该方法可以识别两个流体接触并量化天然气的饱和度。模型确定两个接触点之间的区域为残留气体区域。对浅层气体和古全球变质岩的发生的观察表明,浅层天然气的显示可以作为古近层GWC的指示物。研究得出结论,平整斑应该是针对任何在孟都组中以天然气为勘探目标的主要要求。两个特征流体接触可以通过浅层气的出现来识别,也可以在地震道上被识别。区分两个流体接触的能力将减少定量储量的不确定性。

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