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Geochemical evaluation and hydrocarbon generation potential of the Upper Cretaceous–Pliocene succession, offshore Nile Delta, Egypt

Farouk, Sherif; Khairy, Ahmed; Shehata, Amr M.; Uguna, Clement N.; El Sheennawy, Tamer; Salama, Ahmad; Al-Kahtany, Khaled; Meredith, Will

Geochemical evaluation and hydrocarbon generation potential of the Upper Cretaceous–Pliocene succession, offshore Nile Delta, Egypt Thumbnail


Authors

Sherif Farouk

Ahmed Khairy

Amr M. Shehata

Tamer El Sheennawy

Ahmad Salama

Khaled Al-Kahtany



Abstract

The offshore Nile Delta is a prominent petroleum province; nevertheless, previous research focused mainly on evaluation of Miocene–Pliocene possible source rocks because of lack of data. The current study is the first to evaluate organic geochemical features of the Upper Cretaceous–Pliocene sequence in the western offshore Nile Delta, applying TOC, Rock-Eval pyrolysis and GC-MS procedures for 137 ditch cuttings collected from three wells. The main objectives are to infer organic richness, type of kerogen, maturation, and depositional paleoenvironment of organic matter for these possible source intervals. The analysed rock samples generally display fair to good organic enrichment. Most of these samples are enriched in Type-III and Type-II/III kerogen, suggesting a high influx of terrigenous organic matter. However, Abu Madi, Appollonia, and Khoman formations contain Type-II oil-prone kerogen, reflecting more marine organic matter, whereas Kafr El Sheikh and El Wastani cuttings display the lowest TOC contents and are more enriched in non-generating inert organic matter. Biomarker ratios indicate that Kafr El Sheikh, Abu Madi, Qawasim, and Qantara formations are rich in Type-II/III kerogen (mixed organic matter) preserved under suboxic nearshore or lacustrine depositional environments. In contrast, Sidi Salem, Tineh, Appollonia, and Khoman formations contain abundant Type-II marine-algal organic matter deposited under anoxic marine depositional settings. Vitrinite reflectance data and biomarker ratios indicate immature to peak mature rock samples. The stable carbon isotopic composition of condensate oil samples suggests nonmarine waxy oils. Ratios of n-alkanes and isoprenoids for a condensate sample from the study area reveal no similarity with the Upper Cretaceous–Pliocene rock extracts.

Citation

Farouk, S., Khairy, A., Shehata, A. M., Uguna, C. N., El Sheennawy, T., Salama, A., Al-Kahtany, K., & Meredith, W. (2023). Geochemical evaluation and hydrocarbon generation potential of the Upper Cretaceous–Pliocene succession, offshore Nile Delta, Egypt. Journal of African Earth Sciences, 205, Article 105004. https://doi.org/10.1016/j.jafrearsci.2023.105004

Journal Article Type Article
Acceptance Date Jun 26, 2023
Online Publication Date Jun 28, 2023
Publication Date 2023-09
Deposit Date Jul 17, 2023
Publicly Available Date Jun 29, 2024
Journal Journal of African Earth Sciences
Print ISSN 1464-343X
Electronic ISSN 1879-1956
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 205
Article Number 105004
DOI https://doi.org/10.1016/j.jafrearsci.2023.105004
Keywords Cretaceous–Pliocene Source rocks; Biomarkers; Depositional paleoenvironment; Offshore Nile Delta
Public URL https://nottingham-repository.worktribe.com/output/23206957
Publisher URL https://www.sciencedirect.com/science/article/pii/S1464343X23001772?via%3Dihub

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