Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/3307
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dc.contributor.authorMohamed, Muhammad Azfaren_US
dc.contributor.authorNasir, Mazshurraiezalen_US
dc.contributor.authorSaid, Mohd Syukrien_US
dc.contributor.authorChoong, Chee Mengen_US
dc.contributor.authorSokiman, Mohamad Shaufien_US
dc.contributor.authorMd Akhir, Nur Asyrafen_US
dc.contributor.authorMd Yusof, Muhammad Aslamen_US
dc.contributor.authorZakariah, Muhammad Noor Aminen_US
dc.contributor.authorRashid, Mohd Nizam Abdulen_US
dc.contributor.authorHusein, Salahuddinen_US
dc.contributor.authorSulaiman, N.en_US
dc.contributor.authorMohd, Afiq Naimen_US
dc.date.accessioned2022-09-13T05:06:04Z-
dc.date.available2022-09-13T05:06:04Z-
dc.date.issued2022-06-
dc.identifier.issn25869159-
dc.identifier.urihttp://hdl.handle.net/123456789/3307-
dc.descriptionScopusen_US
dc.description.abstractThis 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 typesen_US
dc.language.isoenen_US
dc.publisherPenerbit UTM Pressen_US
dc.relation.ispartofASEAN Engineering Journalen_US
dc.subjectSemantan Formationen_US
dc.subjectsedimentologicalen_US
dc.subjectchannel-leveeen_US
dc.subjectLobesen_US
dc.subjecthybrid gravity flow depositen_US
dc.subjectCentral of Pahangen_US
dc.titleFacies Analysis and Depositional Model of The Middle-Upper Triassic Semantan Formation, Central Pahang, Malaysiaen_US
dc.typeInternationalen_US
dc.identifier.doi10.11113/aej.V12.17312-
dc.description.page195-203en_US
dc.volume12(2)en_US
dc.description.typeArticleen_US
item.languageiso639-1en-
item.grantfulltextopen-
item.openairetypeInternational-
item.fulltextWith Fulltext-
crisitem.author.deptUNIVERSITI MALAYSIA KELANTAN-
crisitem.author.deptUNIVERSITI MALAYSIA KELANTAN-
Appears in Collections:Faculty of Earth Science - Journal (Scopus/WOS)
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