Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia

The ancient sedimentary rock from the field outcrop gives information on sedimentary features and enhances the depositional environment history. This research incorporated the information on the past sea-level fluctuations of sedimentary rock succession of Perlis area, particularly in Guar Sanai, Ka...

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主要作者:	Zamri, Nurul Syazwin
格式:	Thesis
語言:	English
出版:	2021
主題:	QC1 Physics (General)
在線閱讀:	http://eprints.usm.my/53754/1/NURUL%20SYAZWIN%20BINTI%20ZAMRI%20-%20TESIS24.pdf
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id	my-usm-ep.53754
record_format	uketd_dc
spelling	my-usm-ep.537542022-07-31T18:42:57Z Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia 2021-10 Zamri, Nurul Syazwin QC1 Physics (General) The ancient sedimentary rock from the field outcrop gives information on sedimentary features and enhances the depositional environment history. This research incorporated the information on the past sea-level fluctuations of sedimentary rock succession of Perlis area, particularly in Guar Sanai, Kampung Guar Jentik, and Bukit Tungku Lembu, Beseri area, to verify the events imprinted in the rock record. The data survey was carried out on 10th November 2018 during the mid-semester break. Therefore, this study overview was carried out to analyse the sedimentary facies and reconstruction of the paleo-environment history model for this rock profile via sedimentology logging, facies analysis study, and Fischer plotting analysis. Sedimentological and sequence stratigraphic evidence indicates that the Bukit Tungku Lembu outcrop represents a deposit of coastal, wave, and storm-influenced shoreface shelf system that reflects a shallow marine near fluvial paleo-depositional environment, and the Chuping Formation represents a restricted shallow marine environment. In contrast, the Guar Sanai outcrop represents a deeper marine to shoreface environment with glacial marine deposits. Six sedimentary facies have been recognised in Guar Sanai are which are; (F1) limestone interbedded with black mudstone, (F2) black shale, (F3) black mudstone interbedded with chert, (F4) mudstone, (F5) sandstone, and (F6) diamictite while five sedimentary facies in Bukit Tungku Lembu area which are; (F1) coal, (F2) silty shale, (F3) shale, (F4) sandstone, and (F5) interbedded of sandstone with silty shale and, three sedimentary facies of Chuping Formation which are; (F1) brecciated limestone, (F2) dolomite, and (F3) limestone. 2021-10 Thesis http://eprints.usm.my/53754/ http://eprints.usm.my/53754/1/NURUL%20SYAZWIN%20BINTI%20ZAMRI%20-%20TESIS24.pdf application/pdf en public masters Universiti Sains Malaysia. Pusat Pengajian Sains Fizik
institution	Universiti Sains Malaysia
collection	USM Institutional Repository
language	English
topic	QC1 Physics (General)
spellingShingle	QC1 Physics (General) Zamri, Nurul Syazwin Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia
description	The ancient sedimentary rock from the field outcrop gives information on sedimentary features and enhances the depositional environment history. This research incorporated the information on the past sea-level fluctuations of sedimentary rock succession of Perlis area, particularly in Guar Sanai, Kampung Guar Jentik, and Bukit Tungku Lembu, Beseri area, to verify the events imprinted in the rock record. The data survey was carried out on 10th November 2018 during the mid-semester break. Therefore, this study overview was carried out to analyse the sedimentary facies and reconstruction of the paleo-environment history model for this rock profile via sedimentology logging, facies analysis study, and Fischer plotting analysis. Sedimentological and sequence stratigraphic evidence indicates that the Bukit Tungku Lembu outcrop represents a deposit of coastal, wave, and storm-influenced shoreface shelf system that reflects a shallow marine near fluvial paleo-depositional environment, and the Chuping Formation represents a restricted shallow marine environment. In contrast, the Guar Sanai outcrop represents a deeper marine to shoreface environment with glacial marine deposits. Six sedimentary facies have been recognised in Guar Sanai are which are; (F1) limestone interbedded with black mudstone, (F2) black shale, (F3) black mudstone interbedded with chert, (F4) mudstone, (F5) sandstone, and (F6) diamictite while five sedimentary facies in Bukit Tungku Lembu area which are; (F1) coal, (F2) silty shale, (F3) shale, (F4) sandstone, and (F5) interbedded of sandstone with silty shale and, three sedimentary facies of Chuping Formation which are; (F1) brecciated limestone, (F2) dolomite, and (F3) limestone.
format	Thesis
qualification_level	Master's degree
author	Zamri, Nurul Syazwin
author_facet	Zamri, Nurul Syazwin
author_sort	Zamri, Nurul Syazwin
title	Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia
title_short	Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia
title_full	Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia
title_fullStr	Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia
title_full_unstemmed	Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia
title_sort	recognition of sea-level fluctuations in silurian to permian deposits, perlis, malaysia
granting_institution	Universiti Sains Malaysia.
granting_department	Pusat Pengajian Sains Fizik
publishDate	2021
url	http://eprints.usm.my/53754/1/NURUL%20SYAZWIN%20BINTI%20ZAMRI%20-%20TESIS24.pdf
_version_	1747822259983089664

Recognition Of Sea-level Fluctuations In Silurian To Permian Deposits, Perlis, Malaysia

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