--> Sequence Stratigraphic Analysis of ‘AB’ Field in the NIiger Delta, Nigeria, Using Well Logs and Seismic Data
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2018 AAPG International Conference and Exhibition

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Previous HitSequenceNext Hit Stratigraphic Previous HitAnalysisNext Hit of ‘AB’ Field in the NIiger Delta, Nigeria, Using Previous HitWellNext Hit Logs and Previous HitSeismicNext Hit Data

Abstract

A study was carried out in the ‘AB’ field of the Niger Delta using Previous HitwellNext Hit logs and Previous HitseismicNext Hit data so as to understand the local stratigraphy, identify and describe the sedimentation patterns in the field in order to identify the depositional environments likely to generate hydrocarbon accumulation in the study area. Previous HitSequenceNext Hit stratigraphic framework for ‘AB’ field was constructed by Previous HitcombiningNext Hit Previous HitwellNext Hit Previous HitlogNext Hit data and Previous HitseismicNext Hit volume from three wells in the field. Interpretation of the gamma, resistivity and density logs was done using the petrel software, in which sequences were identified on Previous HitwellNext Hit logs from its trace and Previous HitsequenceNext Hit boundaries. System tracts were used to foretell the reservoir location and quality in order to infer the depositional environment. Key bounding surfaces and depositional sequences were delineated from the Previous HitseismicNext Hit profiles through reflection termination patterns. Results were presented in form of Previous HitwellNext Hit logs, Previous HitseismicNext Hit sections and tables for the 3 wells -A, B and C. 3 sequences were delineated with each of the sequences showing similarities in their Previous HitlogNext Hit signatures to the others. Previous HitLogNext Hit patterns ranges from blocky to serrate, indicating intervals of abrupt decrease in gamma ray Previous HitlogNext Hit response and intervals with increasing response. Previous HitLogNext Hit patterns conform to different environment of deposition in different system tracts, ranging from a basin floor fan in the Low stand to shore face sands and fluvial incisions in the High stand system tracts. Reflection packages observed from the Previous HitseismicNext Hit profiles showed different depositional geometries. Reflection patterns showed variable amplitude from high to low and high to low continuity. The prograding wedge complex is seen as high amplitude parallel reflections, high continuity of reflection patterns indicated uniform deposition of sediments while poor continuity showed non- uniform deposition. Structural Previous HitanalysisNext Hit of the Previous HitseismicTop profiles showed the presence of roll over structures which are good traps for hydrocarbon accumulation. Depth maps showed that the depth to the top of the prospects for the horizons mapped ranges from 4100-5500 feet .The alternation of high stand sands and transgressive shale was inferred to provide the desired combination of seal, source rock and reservoir necessary for hydrocarbon accumulation