Causes and consequences of Oligocene-Miocene relative sea level change in Asia: An example from the Labuan Island (Sabah), Malaysia

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dc.contributor.authorRajat Mazumder
dc.contributor.authorShuvabrata De
dc.contributor.authorBrandon Teo Jun Sien
dc.contributor.authorJeffrey Tang Zhong Heng
dc.contributor.authorOctavian Catuneanu
dc.contributor.authorRenchao Yang
dc.contributor.authorSusan Marriott
dc.coverage.publicationMalaysia
dc.date.accessioned2024-05-14T04:50:46Z
dc.date.available2024-05-14T04:50:46Z
dc.date.issued2021
dc.description.abstractLabuan Island represents the emergent part of a north-eastward plunging anticline. The stratigraphic succession at Labuan is made up of four formations: the Crocker Formation, the Temburong Formation, the Setap shale Formation and the Belait Formation. The sedimentological aspects of the Labuan stratigraphic succession have been studied by several authors but the stratigraphic relationships between the formations is still a matter of conjecture. In this paper we have undertaken an outcrop based (1) sedimentary facies analysis of the Middle Miocene Belait Formation and (2) inferred the mode of stratigraphic sequence building of the Oligocene-Miocene successions.
dc.identifier.citationMazumder, R., De, S., Sien, B. T. J., Heng, J. T. Z., Catuneanu, O., Yang, R., & Marriott, S. (2021). Causes and consequences of Oligocene-Miocene relative sea level change in Asia: An example from the Labuan Island (Sabah), Malaysia. Journal of Asian Earth Sciences, 212, 104746.
dc.identifier.urihttps://repoemc.ukm.my/handle/123456789/661
dc.languageen
dc.publisherElsevier
dc.publisher.alternativeJournal of Asian Earth Sciences
dc.subjectSedimentology
dc.subjectMiocene
dc.subjectBelait Formation
dc.subjectBorneo
dc.subjectStratigraphy
dc.subjectUnconformity
dc.subjectOligocene
dc.titleCauses and consequences of Oligocene-Miocene relative sea level change in Asia: An example from the Labuan Island (Sabah), Malaysia
dc.typeJournal

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