Characterization of Depositional Environments and Hydrocarbon Potential in the AI Well Niger Delta Basin

Authors

  • Efetobore Maju-Oyovwikowhe Department of Geology, Faculty of Physical Science, University of Benin, Benin City, Nigeria https://orcid.org/0000-0001-5041-0524
  • Stephine Aisosa Egharevba Department of Geology, Faculty of Physical Science, University of Benin, Benin City, Nigeria
  • Godwin Okumagbe Aigbadon Department of Geology, Faculty of Physical Science, University of Benin, Benin City, Nigeria
  • Sarah Itohan Aduwa Earth and Environmental Sciences, University of West Florida, USA

Keywords:

Agbada Formation, depositional environment, reservoir quality, petrography, Niger Delta Basin

Abstract

Reservoir characterization is essential for understanding subsurface geology, supporting hydrocarbon exploration, and improving production strategies. This study investigates the AI Well within the Agbada Formation of the Niger Delta Basin through an integrated sedimentological, petrographic, and geochemical approach. A total of 100 ditch cutting samples were analyzed to evaluate lithofacies, mineralogical composition, and geochemical variations. The results indicate a depositional transition from high-energy fluvial to low-energy marine environments, with quartz-rich sandstones serving as primary reservoir units and clay-rich shales acting as effective seals. Petrographic and X-ray diffraction (XRD) analyses show that quartz is the dominant framework mineral, whereas kaolinite and chlorite are associated with reduced porosity and permeability. X-ray fluorescence (XRF) results reveal silica enrichment and ferruginization, indicating post-depositional diagenetic alterations that influence reservoir quality. The findings emphasize that both depositional facies and diagenetic processes play vital roles in controlling reservoir performance. This study underscores the significance of multidisciplinary integration in refining reservoir models and optimizing hydrocarbon recovery in the Niger Delta Basin. 

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Published

2025-12-31

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