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 >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:使用简单的加载模型预测中新世碳酸盐岩勘探目标,卢卡尼亚,砂拉越的地壳孔隙压力

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Miocene carbonate reservoirs form frequentrnexploration targets in basins such as North Lombokrnand Central Luconia, Sarawak. One of the key risksrnassociated with these traps is that of mechanical sealrnfailure, whereby pore pressure at the crest of thernstructure exceeds the fracture strength of the seal.rnTherefore, quantifiying this risk pre-drill can helprnprevent the drilling of dry holes in Luconia,rnSarawak.rnPredicting pore pressure in these basins is hamperedrnby the frontier nature of much of the drilling i.e.rnlittle well calibration and poor/limited seismicrnand/or log data. Moreover, carbonates in general dornnot have a porosity/effective stress relationshiprnwhich enables traditional pressure predictionrntechniques to be used. Therefore, in order to providernaccurate pore pressure for use in estimation ofrnbreach risk, we propose a two step method thatrnrelies on simple loading and required only the usernof chrono-stratigraphic markers derived fromrnseismic.rnStep 1 uses rates of sedimentation and stratigraphicrnages to determine theoretical shale pressure profiles.rnIn thick shale sequences, where disequilibriumrncompaction is the mechanism for generatingrnoverpressure, pore pressure builds parallel to thernloading or evolving overburden. If loading rates arernhigh, then these profiles start at depths less thanrn1.0km. Therefore, using this approach allows us tornproduce a model for shale pressure in these basins.rnThick sand-rich sequences are likely to have lowerrnreservoir (and shale) pressures. As these pinnacle reef targets are steeply inclinedrnby up to 1km of relief, the differential overpressurernin the shales between the crest of any structure andrnthe down-dip spill point can be significant. Thisrndifference in overpressure is transferred to therncarbonate reservoir such that crestal pressure at thernreservoir/seal interface can be elevated in excess ofrnthe surrounding shale pressure. This process isrntermed lateral transfer. Thus, step 2 is to determinernthis additional presssure at the crest and add this tornthe shale pressure as calculated in step 1.rnUsing this simple workflow, a kick taken in CentralrnLuconia well A drilled by SapuraKencana EnergyrnInc. is matched in the post-drill analysis. Moreover,rnthe risk of mechanical seal failure can be morernaccurately addressed. This will help to prevent thernrisk of drilling dry holes in the future. Wherernsufficient seal capacity is demonstrated,rnhydrocarbon column lengths can be calculated.
机译:中新世碳酸盐岩储层在诸如北龙目岛和沙捞越中部卢西亚等盆地形成了频繁的勘探目标。与这些圈闭有关的关键风险之一是机械密封的失效,即结构顶部的孔隙压力超过了密封的断裂强度。因此,对这种风险进行定量分析可以帮助防止在Luconia,Sarawak钻干井。这些盆地的孔隙压力的预测受许多钻井小井定标的前沿性质和不良/局限的地震测井和/或测井数据的阻碍。而且,碳酸盐通常不具有孔隙率/有效应力关系,这使得能够使用传统的压力预测技术。因此,为了提供准确的孔隙压力来估算裂隙风险,我们提出了一种两步法,该方法依靠简单的加载,并且仅需要地震测年地层标记的使用者。第一步:使用沉积速率和地层裂隙率确定理论页岩压力在较厚的页岩层序中,不平衡压实是产生超压的机制,孔隙压力的建立与超载或演化的覆盖层平行。如果加载速率很高,则这些剖面的起始深度小于1.0km。因此,使用这种方法可以使我们在这些盆地中建立页岩压力模型。厚砂富集层可能具有较低的储层(和页岩)压力。由于这些石峰礁目标陡峭地倾斜了1 km,所以任何结构的波峰与下倾溢油点之间的页岩中的压差过大都可能很大。这种超压的差异被传递到碳酸盐储层,使得储层/密封层界面的地壳压力可以升高超过周围的页岩压力。该过程称为横向转移。因此,步骤2是确定在波峰处的该额外压力,并按照步骤1中的计算来添加该页岩压力。使用此简单的工作流程,在SapuraKencana EnergyrnInc钻的CentralLuconia井A中进行一次反冲。在钻后分析中匹配。此外,可以更准确地解决机械密封失效的风险。这将有助于防止将来出现钻干孔的危险。如果显示出足够的密封能力,则可以计算出烃柱的长度。

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