尼日尔三角洲盆地Useni- 1沉积环境与相分析,利用测井、岩心资料

G. Aigbadon, E. O. Akpunonu, S. O. Agunloye, A. Ocheli, O. O .Akakaru
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引用次数: 4

摘要

利用测井资料和岩心相结合的方法,建立了Useni-1油田储层模型。利用岩心资料和测井资料对储层岩石物理特征进行了评价。根据井和岩心资料推断出古沉积环境。沉积相模型显示井所在位置具有高渗透率的通道。环境特征表明,储层为河道相高渗透带。四个储层的深度范围为8000英尺至8400英尺,厚度从20英尺到400英尺不等。岩石物理结果表明,储层孔隙度在12% ~ 28%之间;渗透率145.70 md ~ 454.70md;含水饱和度为21.65% ~ 54.50%,含油饱和度为45.50% ~ 78.50%。岩心资料和伽马测井趋势呈右箱形车趋势,表明下三角洲平原环境中存在河流点坝和潮道充填。在该油田7800 ~ 78100英尺深的低电阻率产砂D1、D2中发现了漏失的油气。
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Depositional Environment and facies analysis of Useni- 1, Niger Delta Basin, using well logs, core data
This study was carried out integrating well logs and core to build reservoir model for the Useni-1 oil field. Core data and well logs were used to evaluate the petrophysical characteristics of the reservoirs. The paleodepositional environment was deduce from the wells and cores data. The depositional facies model showed highly permeable channels where the wells where positioned. The environments identified that the fluvial channel facies with highly permeable zones constituted the reservoirs. Four reservoirs were mapped at depth range of 8000ft to 8400ft with thicknesses varying from 20ft to 400ft. Petrophysical results showed that porosity of the reservoirs varied from 12% to 28 %; permeability from 145.70 md to 454.70md; water saturation from 21.65% to 54.50% and hydrocarbon saturation from 45.50% to 78.50 %. Core data and the gamma ray log trends with right boxcar trend indicate fluvial point bar and tidal channel fills in the lower delta plain setting. By-passed hydrocarbons were identified in low resistivity pay sands D1, D2 at depth of 7800 – 78100ft in the field.  
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