Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam

Eleven Neogene outcrops (seven of the Miri Formation and four of the Seria Formation) from Brunei Darussalam are described. Detailed stratigraphic columns are presented with special emphasis on the sedimentary sequences, providing insights into the depositional environments. The rocks are comprised...

Full description

Main Authors: Roslim, A., Briguglio, A., Kocsis, L., Rahman, F.A., Bahrein, I.F., Goeting, S., Razak, H.
Format: Article
Institution: Universiti Teknologi Petronas
Record Id / ISBN-0: utp-eprints.29819 /
Published: Geological Society of Malaysia 2020
Online Access: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85096984228&doi=10.7186%2fbgsm70202004&partnerID=40&md5=c32fa63724805a24ffcb1728c8cb4aee
http://eprints.utp.edu.my/29819/
Tags: Add Tag
No Tags, Be the first to tag this record!
id utp-eprints.29819
recordtype eprints
spelling utp-eprints.298192022-03-25T02:56:54Z Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam Roslim, A. Briguglio, A. Kocsis, L. Rahman, F.A. Bahrein, I.F. Goeting, S. Razak, H. Eleven Neogene outcrops (seven of the Miri Formation and four of the Seria Formation) from Brunei Darussalam are described. Detailed stratigraphic columns are presented with special emphasis on the sedimentary sequences, providing insights into the depositional environments. The rocks are comprised mostly of sandstone, claystone and a mix of both lithologies, and are piled up in cycles of coarsening upward successions, which are here interpreted as parasequences. Most sections are characterized by abundant and diverse sedimentary structures, reworked fossiliferous deposits and organic fragments such as ambers and wood remains. Certain beds are rich in fossils: among the macrofossils, the most common are bivalves, gastropods and followed by fish remains (teeth and otholiths), crustaceans, corals and echninoderms, which are abundant at specific locations. Among the microfossils, the most common are foraminifera, which are mostly dominated by either rotaliids or textulariids; the most common genera are Ammonia, Elphidium and Trochammina. Porcelaneous and planktonic foraminifera are rare. Ostracods are also found. Ichnofossils are quite abundant in all sections but are represented mostly by Ophiomorpha and Thalassinoides. In view of the observations, the sections are interpreted as evidence of shallow-marine conditions, in which wave, fluvial and tidal actions strongly influenced the depositional environment. In a few cases, deposition of sediment seems to reflect the transition from wave-dominated to tide-dominated conditions. Our findings indicate that in such shallow marine deposits, the interpretation of sediment type and sedimentary structures alone cannot indicate one specific sedimentary environment, but such observations should include palaeontological evidence to generate more accurate palaeoenvironmental reconstructions. Lastly, our results are discussed in relation to the sedimentary evolution of the region. © 2020 Geological Society of Malaysia. All rights reserved. Geological Society of Malaysia 2020 Article NonPeerReviewed https://www.scopus.com/inward/record.uri?eid=2-s2.0-85096984228&doi=10.7186%2fbgsm70202004&partnerID=40&md5=c32fa63724805a24ffcb1728c8cb4aee Roslim, A. and Briguglio, A. and Kocsis, L. and Rahman, F.A. and Bahrein, I.F. and Goeting, S. and Razak, H. (2020) Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam. Bulletin of the Geological Society of Malaysia, 70 . pp. 39-56. http://eprints.utp.edu.my/29819/
institution Universiti Teknologi Petronas
collection UTP Institutional Repository
description Eleven Neogene outcrops (seven of the Miri Formation and four of the Seria Formation) from Brunei Darussalam are described. Detailed stratigraphic columns are presented with special emphasis on the sedimentary sequences, providing insights into the depositional environments. The rocks are comprised mostly of sandstone, claystone and a mix of both lithologies, and are piled up in cycles of coarsening upward successions, which are here interpreted as parasequences. Most sections are characterized by abundant and diverse sedimentary structures, reworked fossiliferous deposits and organic fragments such as ambers and wood remains. Certain beds are rich in fossils: among the macrofossils, the most common are bivalves, gastropods and followed by fish remains (teeth and otholiths), crustaceans, corals and echninoderms, which are abundant at specific locations. Among the microfossils, the most common are foraminifera, which are mostly dominated by either rotaliids or textulariids; the most common genera are Ammonia, Elphidium and Trochammina. Porcelaneous and planktonic foraminifera are rare. Ostracods are also found. Ichnofossils are quite abundant in all sections but are represented mostly by Ophiomorpha and Thalassinoides. In view of the observations, the sections are interpreted as evidence of shallow-marine conditions, in which wave, fluvial and tidal actions strongly influenced the depositional environment. In a few cases, deposition of sediment seems to reflect the transition from wave-dominated to tide-dominated conditions. Our findings indicate that in such shallow marine deposits, the interpretation of sediment type and sedimentary structures alone cannot indicate one specific sedimentary environment, but such observations should include palaeontological evidence to generate more accurate palaeoenvironmental reconstructions. Lastly, our results are discussed in relation to the sedimentary evolution of the region. © 2020 Geological Society of Malaysia. All rights reserved.
format Article
author Roslim, A.
Briguglio, A.
Kocsis, L.
Rahman, F.A.
Bahrein, I.F.
Goeting, S.
Razak, H.
spellingShingle Roslim, A.
Briguglio, A.
Kocsis, L.
Rahman, F.A.
Bahrein, I.F.
Goeting, S.
Razak, H.
Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam
author_sort Roslim, A.
title Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam
title_short Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam
title_full Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam
title_fullStr Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam
title_full_unstemmed Palaeoenvironmental interpretation of late miocene outcrops (Miri and seria formations) along jalan tutong in brunei darussalam
title_sort palaeoenvironmental interpretation of late miocene outcrops (miri and seria formations) along jalan tutong in brunei darussalam
publisher Geological Society of Malaysia
publishDate 2020
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-85096984228&doi=10.7186%2fbgsm70202004&partnerID=40&md5=c32fa63724805a24ffcb1728c8cb4aee
http://eprints.utp.edu.my/29819/
_version_ 1741197304398872576
score 11.62408

Similar Items