INTEGRATION OF LOGS AND SEISMIC DATA FOR DELINEATION OF DEPOSITIONAL ENVIRONMENT OF CLASTIC SEDIMENTS IN TOMBOY FIELD, NIGER DELTA

Diepiriye C. Okujagu, Ada Ruth, Rex Ome
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Abstract

The depositional environment of Clastic sediments in Tomboy Field Onshore Niger Delta were delineated using 3D Seismic and lithological logs. Well log suites from 5 wells comprising Spontaneous potential, Gamma ray, Sonic, Resistivity, Density, and Neutron logs were obtained and analyzed. Reverse estimation was done for the Neutron log and Bulk Density log using volumetric method. Gamma-ray log were used to calibrate Log motifs and correlate sand bodies TMB-01, TMB-02, TMB-03, TMB-04, and TMB-06. Prediction of depositional environment was made through the usage of wireline log shapes of facies combined with result from seismic data. Results of correlation across the five wells showed that. there was continuity at depth interval of 4000-5000ft across the wells as well 3 did not have any gamma information to correlate accros it. The seismic section showed two major growth faults and a channel fill on seismic (inline 5940, crossline1660) between 3.3-3.6ms. According to the paleo-reconstruction from the correlated wells within the tomboy field, the reservoir is made up of sands from fluvial and tidal channels, barrier, and barrier bar. These sand bodies are likely to contain hydrocarbons because of the rollover anticline, which is found at the fault’s downthrown block. This study has revealed that the Clastic sediments in Tomboy Field Onshore Niger Delta were deposited within a predominantly deltaic environment (transitional).
尼日尔三角洲tomboy油田碎屑沉积物沉积环境测井与地震综合圈定
利用三维地震和岩性测井资料对尼日尔三角洲Tomboy油田碎屑沉积环境进行了圈定。获得并分析了5口井的测井资料,包括自然电位、伽马、声波、电阻率、密度和中子测井。利用体积法对中子测井和体积密度测井进行了反演。伽马射线测井用于校正测井基元,并对TMB-01、TMB-02、TMB-03、TMB-04和TMB-06砂体进行关联。利用测井相形态结合地震资料对沉积环境进行了预测。5口井的对比结果表明:在4000-5000英尺的井间有连续性,3井没有任何伽马信息可以相互关联。地震剖面在3.3 ~ 3.6ms之间显示出两条主要生长断层和一条通道填充(线内5940,线外1660)。根据假河油田相关井的古重建,该储层由河流和潮汐河道砂、堰洲和堰洲坝组成。这些砂体很可能含有碳氢化合物,因为在断层的下倾块体上发现了翻转背斜。研究表明,尼日尔三角洲Tomboy油田碎屑沉积处于以三角洲为主的过渡性沉积环境。
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