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DOI | 10.1016/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 |
ISSN | 00128252 |
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 |
推荐引用方式 GB/T 7714 | 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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