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DOI10.1016/j.earscirev.2018.12.006
A new upper Paleogene to Neogene stratigraphy for Sarawak and Labuan in northwestern Borneo: Paleogeography of the eastern Sundaland margin
Hennig-Breitfeld J.; Breitfeld H.T.; Hall R.; BouDagher-Fadel M.; Thirlwall M.
发表日期2019
ISSN00128252
起始页码1
结束页码32
卷号190
英文摘要The Miri Zone in Sarawak contains thick Paleogene to Neogene sedimentary successions that extend offshore into the Sarawak Basin (Balingian and Central Luconia Provinces) and Sabah Basin. Exploration offshore has shown the Sarawak Basin in the South China Sea contains major hydrocarbon reservoirs. The sediments on land are age equivalents of the offshore successions and can be used to provide insights into their sedimentological and stratigraphic relations. However, because the rocks are found in mountainous regions covered by dense rainforest much of the stratigraphy in the Miri Zone is poorly known, as are timings and causes of major unconformities in the region that are essential for understanding the tectonic history, basin development, and sedimentary pathways. In this study we integrate fieldwork, U–Pb zircon dating, biostratigraphy, and light and heavy mineral analyses to present a revised stratigraphy for the region as well as paleogeographic maps, including major paleo-river systems for the main sedimentary basins. Rocks studied include parts of the Cretaceous to Eocene deep marine Rajang Group, fluvial to marginal marine sediments of the Oligocene to Early Miocene Tatau, Buan, Nyalau and Setap Shale Formations, and the Miocene sediments which are assigned to the Balingian, Begrih and Liang Formations in the Mukah-Balingian province, and the Belait Formation on Labuan. There is still much debate about the timings or even existence of some important unconformities offshore, such as the Middle Miocene Unconformity (MMU) and Deep Regional Unconformity (DRU). We propose to avoid the ambiguous time-based terminology that has been used for different events by different authors. Instead, our results from the on-land stratigraphy show two main unconformities in northern Sarawak; one at c. 37 Ma (Rajang Unconformity), marking the change from deep marine to fluvial – marginal marine sedimentation, and another one at c. 17 Ma (Nyalau Unconformity) which is related to widespread uplift in Borneo and changing river systems. © 2018 Elsevier B.V.
关键词Balingian-Luconia ProvinceBorneoMiri ZonePaleogeographyProvenanceRajang UnconformityU-Pb zircon geochronology
英文关键词geochronology; Paleogene; paleogeography; provenance; stratigraphy; unconformity; uranium-lead dating; zircon; Borneo; East Malaysia; Malaysia; Rajang Basin; Sarawak
语种英语
来源期刊Earth Science Reviews
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/203448
作者单位SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, TW20 0EX, United Kingdom; Department of Earth Sciences, University College London, London, WC1H 0BT, United Kingdom; Department of Earth Sciences, Royal Holloway University of London, Egham, TW20 0EX, United Kingdom
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Hennig-Breitfeld J.,Breitfeld H.T.,Hall R.,et al. A new upper Paleogene to Neogene stratigraphy for Sarawak and Labuan in northwestern Borneo: Paleogeography of the eastern Sundaland margin[J],2019,190.
APA Hennig-Breitfeld J.,Breitfeld H.T.,Hall R.,BouDagher-Fadel M.,&Thirlwall M..(2019).A new upper Paleogene to Neogene stratigraphy for Sarawak and Labuan in northwestern Borneo: Paleogeography of the eastern Sundaland margin.Earth Science Reviews,190.
MLA Hennig-Breitfeld J.,et al."A new upper Paleogene to Neogene stratigraphy for Sarawak and Labuan in northwestern Borneo: Paleogeography of the eastern Sundaland margin".Earth Science Reviews 190(2019).
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