Sherif Farouk
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
Authors
Ahmed Khairy
Amr M. Shehata
Dr CLEMENT UGUNA clement.uguna@nottingham.ac.uk
SENIOR RESEARCH FELLOW
Tamer El Sheennawy
Ahmad Salama
Khaled Al-Kahtany
Dr WILLIAM MEREDITH william.meredith@nottingham.ac.uk
ASSOCIATE PROFESSOR
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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