TY  - JOUR
SN  - 25869159
PB  - Penerbit UTM Press
EP  - 203
AV  - none
N1  - cited By 1
TI  - FACIES ANALYSIS AND DEPOSITIONAL MODEL OF THE MIDDLE-UPPER TRIASSIC SEMANTAN FORMATION, CENTRAL PAHANG, MALAYSIA
SP  - 195
Y1  - 2022///
UR  - https://www.scopus.com/inward/record.uri?eid=2-s2.0-85134705915&doi=10.11113%2faej.V12.17312&partnerID=40&md5=20a47342ca1911c84987232a581524e5
JF  - ASEAN Engineering Journal
A1  - Mohamed, M.A.
A1  - Nasir, M.
A1  - Said, M.S.
A1  - Choong, C.M.
A1  - Sokiman, M.S.
A1  - Md Akhir, N.A.
A1  - Md Yusof, M.A.
A1  - Zakariah, M.N.A.
A1  - Rashid, M.N.A.
A1  - Husein, S.
A1  - Sulaiman, N.
A1  - Mohd, A.N.
VL  - 12
N2  - 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. © 2022 Penerbit UTM Press. All rights reserved.
IS  - 2
ID  - scholars16659
ER  -