几内亚湾喀麦隆西南部Rio Del Rey盆地北部海上P10井中新统至新近组储层测井岩性分析及岩石物性参数计算

Romeo Kuete Noupa, Paul Gustave Fowé Kwetche, Steve Imeli Talla, Lawane Esaie Silvere, Joseph Rene Lavenir Binyet Ndjebakal, M. Bessong, M. Ntamak-Nida
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摘要

P10井位于喀麦隆西南部Rio Del Rey盆地北部海域。尽管从南部几个油田的产量来看,Rio Del Rey盆地是喀麦隆最多产的沿海盆地,但其北部的勘探仍然很少。本研究结合了对P10井测井资料的“Quick Look”解释,以及通过中子孔隙度-容重图(NPHI-RHOB)和δ时间声波-容重图(DT-RHOB)对不同岩相进行的“复杂基质”相分析,对盆地北部的石油潜力进行了评价。复合测井包括伽马测井;井径测井;深电阻率测井;中子孔隙度测井和体积密度测井。除了该复合测井外,还完成了井尾地质报告,以完善结果。在950 ~ 1803 TVD m(真垂直深度,单位为米)之间圈定了10个砂/砂岩储层,孔隙度非常好(12% <Φ< 30%),矿物成分以石英为主。除R5和R6储层粘土含量约为24%外,其余储层粘土含量相对低于18%,为砂粘土岩性。R2和R4储层含油,后者的WOC(水油界面)在~1172 m, GOC(气油界面)在1169 m。水库R6;R7;R8;R9机型;R10均含气和水,WGC(水气接触面)位于~1431 m;1530米;分别为1690 m和~1790 m。研究区气态油气藏明显优于油浸油气藏。这项工作提供的结果可以作为未来Rio Del Ray盆地北部油气勘探项目的基线数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Well Log Lithological Analysis and Petrophysical Parameters Calculation of Miocene to Recent Formation Reservoirs in Well P10, Offshore, Northern Rio Del Rey Basin (Southwest Cameroon, Gulf of Guinea)
The P10 well is located offshore, in the Northern part of the Rio Del Rey basin in southwest Cameroon. Although the Rio Del Rey basin is the most prolific coastal basin in Cameroon given the production results from several fields in the southern part, yet it remains very little explored in its northern part. This work evaluation the petroleum potential in the northern part of the Basin using a combination of the "Quick Look" interpretation of the logs recorded in well P10 and "complex matrix" facies analysis of the different lithofacies through the neutron porosity - bulk density (NPHI-RHOB) and delta time sonic - bulk density (DT-RHOB) diagrams. The composite log includes the Gamma Ray log; Caliper log; Deep Resistivity log; neutron porosity log and bulk density log. In addition to this composite log, a geological end of well report is completed to refine the results. Ten (10) near sand/sandstone reservoirs were delineated between 950 and 1803 TVD m (true vertical depth in meter) with very good porosities (12% <Φ< 30%) as well as a mineralogical composition dominated by quartz. Clay volumes are relatively lower than 18% except in reservoirs R5 and R6 where they are around 24%, giving the latter a sandy-clay lithology. Reservoirs R2 and R4 contain oil, the latter with a WOC (Water Oil Contact) at ~1172 m and a GOC (Gas Oil Contact) at 1169 m. Reservoirs R6; R7; R8; R9; R10 all contain Gas and Water with WGC (Water Gas Contact) located at ~1431 m; 1530 m; 1690 m and ~1790 m respectively. In the light of these results, there is a clear dominance of gaseous hydrocarbon reservoirs over oil-impregnated ones in the study area. The results provided by this work can serve as baseline data for future oil and gas exploration projects in the northern part of the Rio Del Ray Basin.
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