Please use this identifier to cite or link to this item:
http://hdl.handle.net/123456789/3307
DC Field | Value | Language |
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dc.contributor.author | Mohamed, Muhammad Azfar | en_US |
dc.contributor.author | Nasir, Mazshurraiezal | en_US |
dc.contributor.author | Said, Mohd Syukri | en_US |
dc.contributor.author | Choong, Chee Meng | en_US |
dc.contributor.author | Sokiman, Mohamad Shaufi | en_US |
dc.contributor.author | Md Akhir, Nur Asyraf | en_US |
dc.contributor.author | Md Yusof, Muhammad Aslam | en_US |
dc.contributor.author | Zakariah, Muhammad Noor Amin | en_US |
dc.contributor.author | Rashid, Mohd Nizam Abdul | en_US |
dc.contributor.author | Husein, Salahuddin | en_US |
dc.contributor.author | Sulaiman, N. | en_US |
dc.contributor.author | Mohd, Afiq Naim | en_US |
dc.date.accessioned | 2022-09-13T05:06:04Z | - |
dc.date.available | 2022-09-13T05:06:04Z | - |
dc.date.issued | 2022-06 | - |
dc.identifier.issn | 25869159 | - |
dc.identifier.uri | http://hdl.handle.net/123456789/3307 | - |
dc.description | Scopus | en_US |
dc.description.abstract | 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). TheSemantan Formation deep-water fan is analysed as a sand-rich fan system, based on its sediment types | en_US |
dc.language.iso | en | en_US |
dc.publisher | Penerbit UTM Press | en_US |
dc.relation.ispartof | ASEAN Engineering Journal | en_US |
dc.subject | Semantan Formation | en_US |
dc.subject | sedimentological | en_US |
dc.subject | channel-levee | en_US |
dc.subject | Lobes | en_US |
dc.subject | hybrid gravity flow deposit | en_US |
dc.subject | Central of Pahang | en_US |
dc.title | Facies Analysis and Depositional Model of The Middle-Upper Triassic Semantan Formation, Central Pahang, Malaysia | en_US |
dc.type | International | en_US |
dc.identifier.doi | 10.11113/aej.V12.17312 | - |
dc.description.page | 195-203 | en_US |
dc.volume | 12(2) | en_US |
dc.description.type | Article | en_US |
item.grantfulltext | open | - |
item.languageiso639-1 | en | - |
item.openairetype | International | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | UNIVERSITI MALAYSIA KELANTAN | - |
crisitem.author.dept | UNIVERSITI MALAYSIA KELANTAN | - |
Appears in Collections: | Faculty of Earth Science - Journal (Scopus/WOS) |
Files in This Item:
File | Description | Size | Format | |
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FACIES ANALYSIS AND DEPOSITIONAL MODEL OF THE MIDDLE-UPPER TRIASSIC SEMANTAN FORMATION CENTRAL PAHANG MALAYSIA.pdf | 2.11 MB | Adobe PDF | View/Open |
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