Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/117021
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Type: Journal article
Title: Late Middle Miocene volcanism in Northwest Borneo, Southeast Asia: implications for tectonics, paleoclimate and stratigraphic marker
Author: Ramkumar, M.
Santosh, M.
Nagarajan, R.
Li, S.
Mathew, M.
Menier, D.
Siddiqui, N.
Rai, J.
Sharma, A.
Farroqui, S.
Poppelreiter, M.
Lai, J.
Prasad, V.
Citation: Palaeogeography, Palaeoclimatology, Palaeoecology, 2018; 490:141-162
Publisher: Elsevier
Issue Date: 2018
ISSN: 0031-0182
1872-616X
Statement of
Responsibility: 
Mu. Ramkumar, M. Santosh, R. Nagarajan, S.S. Li, M. Mathew, D. Menier, N. Siddiqui, J. Rai, A. Sharma, S. Farroqui, M.C. Poppelreiter, J. Lai, V. Prasad
Abstract: Explosive volcanic events often produce pyroclastic materials that can be recognized from the geological record. These discrete pyroclastics form regional marker beds. Here we report the occurrence of a tephra layer interbedded within very thick coal beds near Mukah, Sarawak, Borneo. Traceable for tens of kilometers in the Mukah area of Sarawak, this tephra layer can be considered as regional stratigraphic marker with precise chronostratigraphic control. Systematic sedimentological, mineralogical, geochemical and zircon UPb geochronological studies have revealed a major effusive volcanic event during the latest Middle Miocene, presumably contemporaneous and/or related to a magmatic event of an earlier phase of the Mt. Kinabalu pluton or magmatism in West Sarawak or East Sabah. The volcanic event had promoted catastrophic flooding of coastal swamps and fall-out from the ash clouds that formed a regionally monotonous tephra layer across the Serravallian- Tortonian boundary. In conjunction with the regional occurrences of trap rocks, structural trends and known tectonic events, we constrained the regional depositional environments, and climate. The tephra layer was deposited in a coastal plain-swamp,- seasonal, shallow, high-moderate energy, fluvial channel-lacustrine environmental setting, wherein atmospheric fallout and eroded material from regoliths formed over older basement and volcanic rocks of the hinterland which were mixed to produce the tephra layer. This tephra layer is sandwiched between the very thick coal beds. A pre-existent volcanic chamber that was active for a long time, also experienced periodic explosive activity from probably the same magma chamber and conduit and including a major explosive activity that recycled early-formed crystals and felsic magma (rhyolite-dacite) during the major effusive event are also recognized. Our findings provide robust evidence for the prevalence of intensive chemical weathering under a wet-humid climate, and relative tectonic quiescence before the major effusive event, and the existence of vast, monotonously gently-sloping coastal plains and luxuriant vegetation akin to the present.
Keywords: Volcanic tephra dispersal; zircon geochronology; Middle Miocene tectonics; coastal swamp; paleoclimate; NW Borneo
Rights: © 2017 Elsevier B.V. All rights reserved.
RMID: 0030078270
DOI: 10.1016/j.palaeo.2017.10.022
Appears in Collections:Geology & Geophysics publications

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