Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt

Global sea-level rise during the Early Turonian-Late Cenomanian Bonarelli event resulted in oceanic anoxia and deposition of organic-rich source rocks across Northern Africa, such as the Late Cretaceous Abu Roash-F carbonates. Here, using thin sections, SEM, XRF, standard core analysis, and Rock-Eva...

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Published in:Journal of African Earth Sciences
Main Authors: Farouk, Sherif, Sen, Souvik, Ahmed, Fayez, Qteishat, Abdelrahman, Al-Kahtany, Khaled, Moreno, Hector Marin, Mitra, Sourav, Arafat, Mohamed
Format: Article in Journal/Newspaper
Language:English
Published: 2024
Subjects:
Online Access:https://eprints.soton.ac.uk/490136/
https://eprints.soton.ac.uk/490136/1/ms_clean_copy_AR-F_28April2024.docx
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spelling ftsouthampton:oai:eprints.soton.ac.uk:490136 2024-06-23T07:56:17+00:00 Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt Farouk, Sherif Sen, Souvik Ahmed, Fayez Qteishat, Abdelrahman Al-Kahtany, Khaled Moreno, Hector Marin Mitra, Sourav Arafat, Mohamed 2024-07 text https://eprints.soton.ac.uk/490136/ https://eprints.soton.ac.uk/490136/1/ms_clean_copy_AR-F_28April2024.docx en English eng https://eprints.soton.ac.uk/490136/1/ms_clean_copy_AR-F_28April2024.docx Farouk, Sherif, Sen, Souvik, Ahmed, Fayez, Qteishat, Abdelrahman, Al-Kahtany, Khaled, Moreno, Hector Marin, Mitra, Sourav and Arafat, Mohamed (2024) Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt. Journal of African Earth Sciences, 215, [105272]. (doi:10.1016/j.jafrearsci.2024.105272 <http://dx.doi.org/10.1016/j.jafrearsci.2024.105272>). cc_by_nc_nd_4 Article PeerReviewed 2024 ftsouthampton https://doi.org/10.1016/j.jafrearsci.2024.105272 2024-06-12T00:24:02Z Global sea-level rise during the Early Turonian-Late Cenomanian Bonarelli event resulted in oceanic anoxia and deposition of organic-rich source rocks across Northern Africa, such as the Late Cretaceous Abu Roash-F carbonates. Here, using thin sections, SEM, XRF, standard core analysis, and Rock-Eval pyrolysis data, we examine the petrographic and geochemical properties of the Abu Roash-F (AR-F) carbonate source rocks. These deep marine carbonates consist of dominantly planktonic foraminifera and calcispheres and are classified as wackestone. Extensive micritization, calcite cementation, and ferroan dolomite cement replacement (filling the bioclastic tests and chambers) are identified as the principal diagenetic factors. Core measurements indicate that these carbonates have very low porosity below 3% and horizontal permeability of 0.003 mD (3x10-18 m2), which is also supported by the observed isolated nanopores in SEM. The elemental concentration from the XRF data confirms a highly reducing depositional environment that facilitated the organic richness during the Early Turonian Oceanic Anoxia Event 2 (OAE2). The studied carbonate interval consists of Type-II kerogen in the oil window with a Tmax of about 440 °C and up to 4.2 wt.% TOC indicating ‘fair’ to ‘excellent’ organic richness and a very high probability of active oil generation and expulsion. Following the wireline logs and core data, the self-sourcing unconventional reservoir potential of the AR-F carbonates has been emphasized. Article in Journal/Newspaper Planktonic foraminifera University of Southampton: e-Prints Soton Journal of African Earth Sciences 215 105272
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Global sea-level rise during the Early Turonian-Late Cenomanian Bonarelli event resulted in oceanic anoxia and deposition of organic-rich source rocks across Northern Africa, such as the Late Cretaceous Abu Roash-F carbonates. Here, using thin sections, SEM, XRF, standard core analysis, and Rock-Eval pyrolysis data, we examine the petrographic and geochemical properties of the Abu Roash-F (AR-F) carbonate source rocks. These deep marine carbonates consist of dominantly planktonic foraminifera and calcispheres and are classified as wackestone. Extensive micritization, calcite cementation, and ferroan dolomite cement replacement (filling the bioclastic tests and chambers) are identified as the principal diagenetic factors. Core measurements indicate that these carbonates have very low porosity below 3% and horizontal permeability of 0.003 mD (3x10-18 m2), which is also supported by the observed isolated nanopores in SEM. The elemental concentration from the XRF data confirms a highly reducing depositional environment that facilitated the organic richness during the Early Turonian Oceanic Anoxia Event 2 (OAE2). The studied carbonate interval consists of Type-II kerogen in the oil window with a Tmax of about 440 °C and up to 4.2 wt.% TOC indicating ‘fair’ to ‘excellent’ organic richness and a very high probability of active oil generation and expulsion. Following the wireline logs and core data, the self-sourcing unconventional reservoir potential of the AR-F carbonates has been emphasized.
format Article in Journal/Newspaper
author Farouk, Sherif
Sen, Souvik
Ahmed, Fayez
Qteishat, Abdelrahman
Al-Kahtany, Khaled
Moreno, Hector Marin
Mitra, Sourav
Arafat, Mohamed
spellingShingle Farouk, Sherif
Sen, Souvik
Ahmed, Fayez
Qteishat, Abdelrahman
Al-Kahtany, Khaled
Moreno, Hector Marin
Mitra, Sourav
Arafat, Mohamed
Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt
author_facet Farouk, Sherif
Sen, Souvik
Ahmed, Fayez
Qteishat, Abdelrahman
Al-Kahtany, Khaled
Moreno, Hector Marin
Mitra, Sourav
Arafat, Mohamed
author_sort Farouk, Sherif
title Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt
title_short Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt
title_full Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt
title_fullStr Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt
title_full_unstemmed Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt
title_sort assessment of the upper cretaceous abu roash carbonate source rocks from the beni suef field, western desert, egypt
publishDate 2024
url https://eprints.soton.ac.uk/490136/
https://eprints.soton.ac.uk/490136/1/ms_clean_copy_AR-F_28April2024.docx
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://eprints.soton.ac.uk/490136/1/ms_clean_copy_AR-F_28April2024.docx
Farouk, Sherif, Sen, Souvik, Ahmed, Fayez, Qteishat, Abdelrahman, Al-Kahtany, Khaled, Moreno, Hector Marin, Mitra, Sourav and Arafat, Mohamed (2024) Assessment of the Upper Cretaceous Abu Roash carbonate source rocks from the Beni Suef field, Western Desert, Egypt. Journal of African Earth Sciences, 215, [105272]. (doi:10.1016/j.jafrearsci.2024.105272 <http://dx.doi.org/10.1016/j.jafrearsci.2024.105272>).
op_rights cc_by_nc_nd_4
op_doi https://doi.org/10.1016/j.jafrearsci.2024.105272
container_title Journal of African Earth Sciences
container_volume 215
container_start_page 105272
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