Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman
The Upper Cretaceous Muti Formation was deposited in the Oman Foreland Basin during the obduction of the allochthonous units on the eastern margin of the Arabian Platform. The formation is exposed in various isolated outcrops around Jabal Akhdar Mountain and is located between the Mesozoic platform...
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Sultan Qaboos University, Oman
2024
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ftsultanqaboosun:oai:ojs.pkp.sfu.ca:article/6512 2024-06-02T08:13:26+00:00 Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman Ahmed Attar, Jenan Ahmed Abbasi, Iftikhar Hanif, Muhammad A.K. El-Ghali, Mohamed Al-Sayigh, Abdulrazaq Al-Harthi, Abdul Rahman 2024-04-24 application/pdf https://journals.squ.edu.om/index.php/squjs/article/view/6512 https://doi.org/10.53539/squjs.vol29iss1pp68-85 eng eng Sultan Qaboos University, Oman https://journals.squ.edu.om/index.php/squjs/article/view/6512/4097 https://journals.squ.edu.om/index.php/squjs/article/view/6512 doi:10.53539/squjs.vol29iss1pp68-85 Copyright (c) 2024 Jenan Ahmed Attar, Iftikhar Ahmed Abbasi, Muhammad Hanif, Mohamed A.K. El-Ghali, Abdulrazaq Al-Sayigh, Abdul Rahman Al-Harthi http://creativecommons.org/licenses/by-nd/4.0 Sultan Qaboos University Journal for Science [SQUJS]; Vol. 29 No. 1 (2024); 68-85 2414-536X 1027-524X info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 2024 ftsultanqaboosun https://doi.org/10.53539/squjs.vol29iss1pp68-85 2024-05-06T17:11:17Z The Upper Cretaceous Muti Formation was deposited in the Oman Foreland Basin during the obduction of the allochthonous units on the eastern margin of the Arabian Platform. The formation is exposed in various isolated outcrops around Jabal Akhdar Mountain and is located between the Mesozoic platform carbonates below and the allochthonous nappe above. The current study is the first to describe the outcrops of the Muti Formation in the Nakhal area. It focuses on the lithofacies, microfacies distribution, and the characterization of the depositional environment of the formation. The lithofacies and microfacies of the formation are described from two measured sections in the study area. The Nakhal section is about 50 m thick and consists of four lithofacies: marl, bedded limestone, nodular limestone, and clay. A total of four microfacies are identified, including echinoderm-spine wackestone, bioclastic packestone, arenaceous wackestone, and mudstone. Diagenetic features such as fractures, cementations, and dissolutions, and their products, for instance, porosities, were also identified, and their paragenetic history was reconstructed. Additionally, microfossils, such as bryozoan fragments, calcispheres, bivalves, fragments of echinoids, and brachiopod fragments, benthic and planktonic foraminifera were recognized. Based on lithological and biotic variations, it is suggested that the Muti Formation in the Nakhal area was deposited in a shallow marine environment on the outer to the mid-carbonate shelves. This formation is subjected to diagenetic changes starting with eogenesis in marine settings followed by burial diagenesis, and subsequently, the formation is exposed to the telogenetic diagenesis phase. Keywords: Muti Formation, Nakhal Area, Oman Foreland Basin, Upper Cretaceous, Jabal Akhdar. Article in Journal/Newspaper Planktonic foraminifera Sultan Qaboos University Scientific Journals Sultan Qaboos University Journal for Science [SQUJS] 29 1 68 85 |
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Sultan Qaboos University Scientific Journals |
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ftsultanqaboosun |
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English |
description |
The Upper Cretaceous Muti Formation was deposited in the Oman Foreland Basin during the obduction of the allochthonous units on the eastern margin of the Arabian Platform. The formation is exposed in various isolated outcrops around Jabal Akhdar Mountain and is located between the Mesozoic platform carbonates below and the allochthonous nappe above. The current study is the first to describe the outcrops of the Muti Formation in the Nakhal area. It focuses on the lithofacies, microfacies distribution, and the characterization of the depositional environment of the formation. The lithofacies and microfacies of the formation are described from two measured sections in the study area. The Nakhal section is about 50 m thick and consists of four lithofacies: marl, bedded limestone, nodular limestone, and clay. A total of four microfacies are identified, including echinoderm-spine wackestone, bioclastic packestone, arenaceous wackestone, and mudstone. Diagenetic features such as fractures, cementations, and dissolutions, and their products, for instance, porosities, were also identified, and their paragenetic history was reconstructed. Additionally, microfossils, such as bryozoan fragments, calcispheres, bivalves, fragments of echinoids, and brachiopod fragments, benthic and planktonic foraminifera were recognized. Based on lithological and biotic variations, it is suggested that the Muti Formation in the Nakhal area was deposited in a shallow marine environment on the outer to the mid-carbonate shelves. This formation is subjected to diagenetic changes starting with eogenesis in marine settings followed by burial diagenesis, and subsequently, the formation is exposed to the telogenetic diagenesis phase. Keywords: Muti Formation, Nakhal Area, Oman Foreland Basin, Upper Cretaceous, Jabal Akhdar. |
format |
Article in Journal/Newspaper |
author |
Ahmed Attar, Jenan Ahmed Abbasi, Iftikhar Hanif, Muhammad A.K. El-Ghali, Mohamed Al-Sayigh, Abdulrazaq Al-Harthi, Abdul Rahman |
spellingShingle |
Ahmed Attar, Jenan Ahmed Abbasi, Iftikhar Hanif, Muhammad A.K. El-Ghali, Mohamed Al-Sayigh, Abdulrazaq Al-Harthi, Abdul Rahman Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman |
author_facet |
Ahmed Attar, Jenan Ahmed Abbasi, Iftikhar Hanif, Muhammad A.K. El-Ghali, Mohamed Al-Sayigh, Abdulrazaq Al-Harthi, Abdul Rahman |
author_sort |
Ahmed Attar, Jenan |
title |
Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman |
title_short |
Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman |
title_full |
Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman |
title_fullStr |
Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman |
title_full_unstemmed |
Lithostratigraphy and Microfacies of the Upper Cretaceous Muti Formation of the Oman Foreland Basin, Nakhal Area, Oman |
title_sort |
lithostratigraphy and microfacies of the upper cretaceous muti formation of the oman foreland basin, nakhal area, oman |
publisher |
Sultan Qaboos University, Oman |
publishDate |
2024 |
url |
https://journals.squ.edu.om/index.php/squjs/article/view/6512 https://doi.org/10.53539/squjs.vol29iss1pp68-85 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Sultan Qaboos University Journal for Science [SQUJS]; Vol. 29 No. 1 (2024); 68-85 2414-536X 1027-524X |
op_relation |
https://journals.squ.edu.om/index.php/squjs/article/view/6512/4097 https://journals.squ.edu.om/index.php/squjs/article/view/6512 doi:10.53539/squjs.vol29iss1pp68-85 |
op_rights |
Copyright (c) 2024 Jenan Ahmed Attar, Iftikhar Ahmed Abbasi, Muhammad Hanif, Mohamed A.K. El-Ghali, Abdulrazaq Al-Sayigh, Abdul Rahman Al-Harthi http://creativecommons.org/licenses/by-nd/4.0 |
op_doi |
https://doi.org/10.53539/squjs.vol29iss1pp68-85 |
container_title |
Sultan Qaboos University Journal for Science [SQUJS] |
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29 |
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1 |
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68 |
op_container_end_page |
85 |
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1800736947890552832 |