Geochemical characterization of the source rock intervals, Beni-Suef Basin, West Nile Valley, Egypt
Author:
Affiliation:
1. Geology Department, Faculty of Sciences, Helwan University , Cairo , Egypt
2. Exploration Department, Agiba Petroleum Company, Nasr City , Cairo , Egypt
Abstract
Publisher
Walter de Gruyter GmbH
Subject
General Earth and Planetary Sciences,Environmental Science (miscellaneous)
Link
https://www.degruyter.com/document/doi/10.1515/geo-2020-0306/pdf
Reference40 articles.
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2. Shehata AA, El Fawal FM, Ito M, Aboulmagd MA, Brooks HL. Senonian platform-to-slope evolution in the tectonically-influenced Syrian Arc sedimentary belt: Beni Suef Basin, Egypt. J Afr Earth Sci. 2020;170:103–34.
3. Makky AF, El Sayed MI, El-Ata ASA, Abd El-Gaied IM, Abdel-Fattah MI, Abd-Allah ZM. Source rock evaluation of some upper and lower cretaceous sequences, West Beni Suef concession, Western Desert, Egypt. Egypt J Pet. 2014;23(1):135–49.
4. Shehata AA, El Fawal FM, Ito M, Aal MHA, Sarhan MA. Sequence stratigraphic evolution of the syn-rift Early Cretaceous sediments, West Beni Suef Basin, the Western Desert of Egypt with remarks on its hydrocarbon accumulations. Arab J Geosci. 2018;11(12):1–18.
5. Bosworth W, El-Hawat AS, Helgeson DE, Burke K. Cyrenaican “shock absorber” and associated inversion strain shadow in the collision zone of northeast Africa. Geology. 2008;36(9):695–8.
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