Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictions

The relationship between quartz surface textural defects (derived from weathering and diagenesis), palaeo-depositional environment and reservoir quality were studied using Tertiary outcrop rock samples obtained from the Belait and Lambir formations of the Sarawak Basin, Malaysia. Thin sections were...

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Main Authors: Abdullah Musa Ali, Eswaran Padmanabhan
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2014-12-01
Series:Petroleum Exploration and Development
Online Access:http://www.sciencedirect.com/science/article/pii/S1876380414600902
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author Abdullah Musa Ali
Eswaran Padmanabhan
author_facet Abdullah Musa Ali
Eswaran Padmanabhan
author_sort Abdullah Musa Ali
collection DOAJ
description The relationship between quartz surface textural defects (derived from weathering and diagenesis), palaeo-depositional environment and reservoir quality were studied using Tertiary outcrop rock samples obtained from the Belait and Lambir formations of the Sarawak Basin, Malaysia. Thin sections were used for mineral identification and to make observations regarding grain size and texture. Morphological characterization of the samples was performed using scanning electron microscopy (SEM) attached with energy-dispersive X-ray spectrometry (EDX) system, to show variations in quartz surface texture. The SEM images of Belait conglomerates reveal euhedral quartz crystals characterized with prominent mechanical weathering defects (such as straight and conchoidal fractures and striations). Conversely, the analysis of the Lambir sandstones identified chemical weathering features (such as chemical etchings, pitting, solution pits and notches). On the basis of petrology, SEM and CT scan images, evaluation results of reservoir quality indicate that the Lambir Formation in this study area is high-energy coast deposit, with apparent tide-dominated features; while Belait Formation is neritic-delta deposit, with obvious wave-dominated features; reservoir quality of the Belait Formation and Lambir Formation are poor, but the porosity of the Belait Formation is relatively higher than that of the Lambir Formation. Key words: Sarawak Basin, quartz morphology, scanning electron microscopy (SEM), microtextures, paleo-depositional environment, reservoir quality
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spelling doaj.art-1f0f5af93ecb4b5ea83545ac21bb424a2022-12-21T18:30:34ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042014-12-01416761770Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictionsAbdullah Musa Ali0Eswaran Padmanabhan1Corresponding author; Department of Geosciences, Faculty of Geosciences and Petroleum Engineering, Universiti Teknologi PETRONAS (UTP), Tronoh, Perak, MalaysiaDepartment of Geosciences, Faculty of Geosciences and Petroleum Engineering, Universiti Teknologi PETRONAS (UTP), Tronoh, Perak, MalaysiaThe relationship between quartz surface textural defects (derived from weathering and diagenesis), palaeo-depositional environment and reservoir quality were studied using Tertiary outcrop rock samples obtained from the Belait and Lambir formations of the Sarawak Basin, Malaysia. Thin sections were used for mineral identification and to make observations regarding grain size and texture. Morphological characterization of the samples was performed using scanning electron microscopy (SEM) attached with energy-dispersive X-ray spectrometry (EDX) system, to show variations in quartz surface texture. The SEM images of Belait conglomerates reveal euhedral quartz crystals characterized with prominent mechanical weathering defects (such as straight and conchoidal fractures and striations). Conversely, the analysis of the Lambir sandstones identified chemical weathering features (such as chemical etchings, pitting, solution pits and notches). On the basis of petrology, SEM and CT scan images, evaluation results of reservoir quality indicate that the Lambir Formation in this study area is high-energy coast deposit, with apparent tide-dominated features; while Belait Formation is neritic-delta deposit, with obvious wave-dominated features; reservoir quality of the Belait Formation and Lambir Formation are poor, but the porosity of the Belait Formation is relatively higher than that of the Lambir Formation. Key words: Sarawak Basin, quartz morphology, scanning electron microscopy (SEM), microtextures, paleo-depositional environment, reservoir qualityhttp://www.sciencedirect.com/science/article/pii/S1876380414600902
spellingShingle Abdullah Musa Ali
Eswaran Padmanabhan
Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictions
Petroleum Exploration and Development
title Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictions
title_full Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictions
title_fullStr Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictions
title_full_unstemmed Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictions
title_short Quartz surface morphology of Tertiary rocks from North East Sarawak, Malaysia: Implications for paleo-depositional environment and reservoir rock quality predictions
title_sort quartz surface morphology of tertiary rocks from north east sarawak malaysia implications for paleo depositional environment and reservoir rock quality predictions
url http://www.sciencedirect.com/science/article/pii/S1876380414600902
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AT eswaranpadmanabhan quartzsurfacemorphologyoftertiaryrocksfromnortheastsarawakmalaysiaimplicationsforpaleodepositionalenvironmentandreservoirrockqualitypredictions