Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia
This study details the sedimentological analysis of the Middle-Upper Triassic Semantan Formation in the Jerantut-Temerloh-Kemayan region of central Pahang. Seven (F1-7) facies have been identified which are; F1) poorly sorted conglomerate, F2) pebbly sandstone, F3) structureless-to-parallel laminate...
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Format: | Article |
Language: | English English |
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Penerbit UTM Press
2022
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Online Access: | http://umpir.ump.edu.my/id/eprint/42662/1/Facies%20analysis%20and%20depositional%20model%20of%20the%20middle-upper%20triassic.pdf http://umpir.ump.edu.my/id/eprint/42662/2/Facies%20analysis%20and%20depositional%20model%20of%20the%20middle-upper%20triassic%20Semantan%20formation%2C%20Central%20Pahang%2C%20Malaysia_ABS.pdf |
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author | Muhammad Azfar, Mohamed Mazshurraiezal, Nasir Mohd Syukri, Said Meng, Choongchee Mohamad Shaufi, Sokiman Nur Asyraf, Md Akhir Muhammad Aslam, Md Yusof Muhammad Noor Amin, Zakariah Mohd Nizam, Abdul Rashid Salahuddin, Husein Noorzamzarina, Sulaiman Afiq Naim, Mohd |
author_facet | Muhammad Azfar, Mohamed Mazshurraiezal, Nasir Mohd Syukri, Said Meng, Choongchee Mohamad Shaufi, Sokiman Nur Asyraf, Md Akhir Muhammad Aslam, Md Yusof Muhammad Noor Amin, Zakariah Mohd Nizam, Abdul Rashid Salahuddin, Husein Noorzamzarina, Sulaiman Afiq Naim, Mohd |
author_sort | Muhammad Azfar, Mohamed |
collection | UMP |
description | This study details the sedimentological analysis of the Middle-Upper Triassic Semantan Formation in the Jerantut-Temerloh-Kemayan region of central Pahang. Seven (F1-7) facies have been identified which are; F1) poorly sorted conglomerate, F2) pebbly sandstone, F3) structureless-to-parallel laminated sandstone, F4) wavy-to-ripple fine-to-medium laminated sandstone, F5) slumped thin-interbeded sandstone and shale, F6) interbedded sandstone and shale, and F7) shale, represent a subordinate part of the Semantan Formation. Examination of the succession of the vertical facies resulted in concession of genetic units (FA1-FA5) which are; FA1) deep channel complex, FA2) distal lobe, FA3) hybrid gravity flow deposit, FA4) channelised lobe and FA5) non-channelised lobe. It is believed that these five genetic units were deposited within four proposed laterally contiguous depositional environments which are; 1) Inner fan - deep channel-levee complex (represent by FA1), 2) Mid fan - channelised lobe (represented by FA5 and FA3), 3) Mid Fan - non-channelised lobe (represented by FA4 and FA3), and 4) Outer fan - distal lobe (represented by FA2). The Semantan Formation deep-water fan is analysed as a sand-rich fan system, based on its sediment types. |
first_indexed | 2025-02-19T02:37:45Z |
format | Article |
id | UMPir42662 |
institution | Universiti Malaysia Pahang |
language | English English |
last_indexed | 2025-02-19T02:37:45Z |
publishDate | 2022 |
publisher | Penerbit UTM Press |
record_format | dspace |
spelling | UMPir426622025-01-07T03:48:00Z http://umpir.ump.edu.my/id/eprint/42662/ Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia Muhammad Azfar, Mohamed Mazshurraiezal, Nasir Mohd Syukri, Said Meng, Choongchee Mohamad Shaufi, Sokiman Nur Asyraf, Md Akhir Muhammad Aslam, Md Yusof Muhammad Noor Amin, Zakariah Mohd Nizam, Abdul Rashid Salahuddin, Husein Noorzamzarina, Sulaiman Afiq Naim, Mohd TA Engineering (General). Civil engineering (General) This study details the sedimentological analysis of the Middle-Upper Triassic Semantan Formation in the Jerantut-Temerloh-Kemayan region of central Pahang. Seven (F1-7) facies have been identified which are; F1) poorly sorted conglomerate, F2) pebbly sandstone, F3) structureless-to-parallel laminated sandstone, F4) wavy-to-ripple fine-to-medium laminated sandstone, F5) slumped thin-interbeded sandstone and shale, F6) interbedded sandstone and shale, and F7) shale, represent a subordinate part of the Semantan Formation. Examination of the succession of the vertical facies resulted in concession of genetic units (FA1-FA5) which are; FA1) deep channel complex, FA2) distal lobe, FA3) hybrid gravity flow deposit, FA4) channelised lobe and FA5) non-channelised lobe. It is believed that these five genetic units were deposited within four proposed laterally contiguous depositional environments which are; 1) Inner fan - deep channel-levee complex (represent by FA1), 2) Mid fan - channelised lobe (represented by FA5 and FA3), 3) Mid Fan - non-channelised lobe (represented by FA4 and FA3), and 4) Outer fan - distal lobe (represented by FA2). The Semantan Formation deep-water fan is analysed as a sand-rich fan system, based on its sediment types. Penerbit UTM Press 2022-06 Article PeerReviewed pdf en http://umpir.ump.edu.my/id/eprint/42662/1/Facies%20analysis%20and%20depositional%20model%20of%20the%20middle-upper%20triassic.pdf pdf en http://umpir.ump.edu.my/id/eprint/42662/2/Facies%20analysis%20and%20depositional%20model%20of%20the%20middle-upper%20triassic%20Semantan%20formation%2C%20Central%20Pahang%2C%20Malaysia_ABS.pdf Muhammad Azfar, Mohamed and Mazshurraiezal, Nasir and Mohd Syukri, Said and Meng, Choongchee and Mohamad Shaufi, Sokiman and Nur Asyraf, Md Akhir and Muhammad Aslam, Md Yusof and Muhammad Noor Amin, Zakariah and Mohd Nizam, Abdul Rashid and Salahuddin, Husein and Noorzamzarina, Sulaiman and Afiq Naim, Mohd (2022) Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia. ASEAN Engineering Journal, 12 (2). pp. 195-203. ISSN 2586-9159. (Published) https://doi.org/10.11113/aej.V12.17312 https://doi.org/10.11113/aej.V12.17312 |
spellingShingle | TA Engineering (General). Civil engineering (General) Muhammad Azfar, Mohamed Mazshurraiezal, Nasir Mohd Syukri, Said Meng, Choongchee Mohamad Shaufi, Sokiman Nur Asyraf, Md Akhir Muhammad Aslam, Md Yusof Muhammad Noor Amin, Zakariah Mohd Nizam, Abdul Rashid Salahuddin, Husein Noorzamzarina, Sulaiman Afiq Naim, Mohd Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia |
title | Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia |
title_full | Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia |
title_fullStr | Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia |
title_full_unstemmed | Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia |
title_short | Facies analysis and depositional model of the middle-upper triassic Semantan formation, Central Pahang, Malaysia |
title_sort | facies analysis and depositional model of the middle upper triassic semantan formation central pahang malaysia |
topic | TA Engineering (General). Civil engineering (General) |
url | http://umpir.ump.edu.my/id/eprint/42662/1/Facies%20analysis%20and%20depositional%20model%20of%20the%20middle-upper%20triassic.pdf http://umpir.ump.edu.my/id/eprint/42662/2/Facies%20analysis%20and%20depositional%20model%20of%20the%20middle-upper%20triassic%20Semantan%20formation%2C%20Central%20Pahang%2C%20Malaysia_ABS.pdf |
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