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首页> 外文期刊>Journal of Geology & Geophysics >Seismic Stratigraphic and Petrophysical Characterization of Reservoirs of the Agbada Formation in the Vicinity of ?¢????Well M?¢????, Offshore Eastern Niger Delta Basin, Nigeria
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Seismic Stratigraphic and Petrophysical Characterization of Reservoirs of the Agbada Formation in the Vicinity of ?¢????Well M?¢????, Offshore Eastern Niger Delta Basin, Nigeria

机译:尼日利亚尼日尔三角洲近海东岸阿格巴达组储层的地震地层和岩石物理特征

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Two dimensional seismic and composite well logs from well M in the eastern offshore Niger delta basin were used to carry out a seismic stratigraphic and petrophysical characterization of reservoirs of the Agbada Formation. Three seismic sequences have been delineated within a time window of 600 ms-2200 ms showing depositional environments that have prograded from the delta platform in seismic sequence one (S1) down to the wave dominated prodelta /slope in seismic sequences three (S3). Five seismic facies (F1, F2, F3, F4, and F5) have been mapped within the study area with F2, the hydrocarbon habitat, consisting of deltaic distributary channel fills. The deposits of F2 were formed during aggradation to progradation of the delta and are considered to be High stand system tracts (HST) reservoirs. Twenty reservoirs zones (A-T) were identified with porosity ranging from 0.192 to 0.423 and permeability from 5.078 to 12,397.895 md, indicating very good porosity and permeability as a result of the low shale volume (0.031-0.148). The values for the bulk volume water are constant or nearly constant throughout the reservoirs and the reservoirs are said to be at irreducible water saturation implying the reservoir can produce water free hydrocarbon hence they are very good hydrocarbon reservoirs. The reservoirs qualities of well M are good and some of the reservoirs are petroliferous. Therefore, Well M could serve as a control well in hydrocarbon exploration in the offshore depobelt.
机译:利用尼日尔三角洲东部近海M井的二维地震和复合测井资料对阿格巴达组储层进行了地震地层和岩石物理表征。在600毫秒至2200毫秒的时间窗口内划定了三个地震序列,显示了从地震序列一(S1)的三角洲平台升至地震序列三(S3)的以波浪为主的三角洲/坡度的沉积环境。研究区域内已绘制了五个地震相(F1,F2,F3,F4和F5),其中F2是烃类生境,由三角洲分流河道填充物组成。 F2的沉积物是在三角洲的渐增和渐进过程中形成的,被认为是高位系统域(HST)储层。确定了二十个储层带(A-T),孔隙度范围为0.192至0.423,渗透率范围为5.078至12,397.895 md,这是由于页岩体积低(0.031-0.148)导致的很好的孔隙度和渗透率。在整个储层中,总体积水的值是恒定的或几乎恒定的,据说这些储层处于不可还原的水饱和状态,这意味着该储层可以生产无水烃,因此它们是非常好的烃储层。 M井的储层质量良好,有些储层是含油的。因此,M井可作为海上沉积带油气勘探的控制井。

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