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:尼日利亚海上东部尼日尔三角洲盆地的Agbada agity的地震地层和岩石物理表征。

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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:从东部尼日尔三角洲盆地的井中的MORY MORY MOTE的二维地震和复合井测井用于开展agbada地层的地震地层和岩石物理表征。在600 ms-2200ms的时间窗口中显示了三个地震序列,示出了从地震序列(S1)中的δ平台上促成的沉积环境,其下降到地震序列中的波导序列三(S3)。五个地震相(F1,F2,F3,F4和F5)已在具有F2,烃栖息地的研究区域内映射,由Celtaic分布通道填充组成。在综合期间形成F2的沉积,以促进三角洲,并且被认为是高支架系统散布(HST)储层。二十个储层区(A-T)用孔隙率鉴定为0.192至0.423和5.078至12,397.895md的渗透率,表明由于低页岩体积(0.031-0.148)而产生非常好的孔隙率和渗透性。在整个储存器中,散装量水的值是恒定的或几乎恒定,并且据说储存器处于不可约的水饱和度,暗示储存器可以产生不含水的烃,因此它们是非常好的碳氢化合物储层。井的水库品质好,一些水库是凡士酒。因此,井M可以作为离岸Dropelt中的碳氢化合物勘探中的控制良好。

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