首页> 外文会议>Indonesian Petroleum Association Convention and Exhibition >USING SIMPLE LOADING MODELS TO PREDICT CRESTAL PORE PRESSURES IN MIOCENE CARBONATE EXPLORATION TARGETS, LUCONIA, SARAWAK
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USING SIMPLE LOADING MODELS TO PREDICT CRESTAL PORE PRESSURES IN MIOCENE CARBONATE EXPLORATION TARGETS, LUCONIA, SARAWAK

机译:使用简单的装载模型来预测中烯碳酸酯勘探靶标中的壁挂孔压力,卢康吡康,沙捞越

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Miocene carbonate reservoirs form frequent exploration targets in basins such as North Lombok and Central Luconia, Sarawak. One of the key risks associated with these traps is that of mechanical seal failure, whereby pore pressure at the crest of the structure exceeds the fracture strength of the seal. Therefore, quantifiying this risk pre-drill can help prevent the drilling of dry holes in Luconia, Sarawak. Predicting pore pressure in these basins is hampered by the frontier nature of much of the drilling i.e. little well calibration and poor/limited seismic and/or log data. Moreover, carbonates in general do not have a porosity/effective stress relationship which enables traditional pressure prediction techniques to be used. Therefore, in order to provide accurate pore pressure for use in estimation of breach risk, we propose a two step method that relies on simple loading and required only the use of chrono-stratigraphic markers derived from seismic. Step 1 uses rates of sedimentation and stratigraphic ages to determine theoretical shale pressure profiles. In thick shale sequences, where disequilibrium compaction is the mechanism for generating overpressure, pore pressure builds parallel to the loading or evolving overburden. If loading rates are high, then these profiles start at depths less than 1.0km. Therefore, using this approach allows us to produce a model for shale pressure in these basins. Thick sand-rich sequences are likely to have lower reservoir (and shale) pressures. As these pinnacle reef targets are steeply inclined by up to 1km of relief, the differential overpressure in the shales between the crest of any structure and the down-dip spill point can be significant. This difference in overpressure is transferred to the carbonate reservoir such that crestal pressure at the reservoir/seal interface can be elevated in excess of the surrounding shale pressure. This process is termed lateral transfer. Thus, step 2 is to determine this additional presssure at the crest and add this to the shale pressure as calculated in step 1. Using this simple workflow, a kick taken in Central Luconia well A drilled by SapuraKencana Energy Inc. is matched in the post-drill analysis. Moreover, the risk of mechanical seal failure can be more accurately addressed. This will help to prevent the risk of drilling dry holes in the future. Where sufficient seal capacity is demonstrated, hydrocarbon column lengths can be calculated.
机译:中新统碳酸盐岩储层形成这样的盆地北龙目岛和中部Luconia,沙捞越频繁的勘探目标。一个主要风险与这些陷阱相关联的是,机械密封失效,从而在该结构的波峰孔隙压力超过密封的断裂强度的。因此,quantifiying这种风险预钻有助于预防Luconia,沙捞越干井的钻探。在这些盆地预测孔隙压力是由多钻井即小以及校准和/差的前沿性质妨碍了限制地震和/或记录数据。此外,在一般的碳酸盐不具有的孔隙率/有效应力关系,其使得能够使用传统的压力的预测技术。因此,为了提供作为违约风险的估计中使用精确的孔隙压力,我们建议,依靠简单的加载并只需要利用地震衍生计时 - 地层标志的两步法。分步沉淀和地层年龄1用途率确定的理论页岩压力分布。在厚页岩序列,其中均衡压实是用于产生超压的机构,孔隙压力建立平行于装载或演变的覆盖层。如果负荷率很高,那么这些配置在深度开始小于1.0公里。因此,使用这种方法可以让我们产生了这些盆地页岩压力的典范。厚富砂的序列很可能有下水库(页岩)的压力。由于这些巅峰礁指标均急剧高达救济1公里倾斜,在任何结构的顶部和下倾溢出点之间的页岩差过压可以显著。在过压的这种差异被转移到所述碳酸盐岩储层,使得在储存器/密封界面脊压力可以过量周边页岩压力的升高。这个过程被称为横向转移。因此,步骤2是在波峰,以确定该附加presssure和将其添加到页岩压力如在步骤1中计算使用这种简单的工作流,在中央Luconia以及A截取的踢钻出通过SapuraKencana能源公司在后匹配 - 打磨分析。此外,机械密封失效的风险可以更准确地解决。这将有助于防止今后钻干井的风险。其中证明足够的密封能力,烃列长度可以计算出来。

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