International Journal of Geosciences

Volume 12, Issue 6 (June 2021)

ISSN Print: 2156-8359   ISSN Online: 2156-8367

Google-based Impact Factor: 0.56  Citations  h5-index & Ranking

Geochemical Evaluation for the Hydrocarbon Potential of Source Rocks in the Anza Basin

HTML  XML Download Download as PDF (Size: 3360KB)  PP. 572-583  
DOI: 10.4236/ijg.2021.126032    252 Downloads   1,627 Views  Citations

ABSTRACT

Anza basin is located in the extensional arm of the central African rift system in the North-Eastern part of Kenya. Cretaceous sedimentary rocks were sampled from the four wells namely, Chalbi-3, Sirius-1, Ndovu-1 and Kaisut-1. Anza basin occurs on a fault block within a Paleocene-Cretaceous rift basin. The methodological approach used for the evaluation of source rocks included petrophysical and geochemical methods to ascertain their potential. Well sections with a higher shale-volume ratio were sampled for geochemical screening to determine the organic richness and thermal maturity of potential source rocks, respectively. Source rock with organic richness ≥ 0.5% were evaluated further for their petroleum potential using Rock-Eval pyrolysis to determine their thermal maturity, organo-facies and in-situ generated hydrocarbons present in sedimentary facies. The geochemical evaluation of rock samples from the drilled wells’ sections of Chalbi-3 and Sirius-1 confirmed both oil and gas potential. Gas Chromatography and Mass Spectrometry (GCMS) were used to characterize the biomarker signatures and oil-oil correlation of Sirius-1 samples. A predictive model was developed to integrate the petrophysical and geochemical data to reveal hydrocarbons’ potential in the Anza basin.

Share and Cite:

Gilbert, B. , Olago, D. , Ichangi, D. and Rop, B. (2021) Geochemical Evaluation for the Hydrocarbon Potential of Source Rocks in the Anza Basin. International Journal of Geosciences, 12, 572-583. doi: 10.4236/ijg.2021.126032.

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.