An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospect

Abstract An overview and integration of key petroleum exploration findings in the onshore Central Sarawak Basin, NW Borneo in the last 2 decades is presented. Findings revealed that critical moments for the generation and preservation of hydrocarbon may be found in the Early Oligocene, Early Miocene...

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Main Authors: Ekundayo Joseph Adepehin, Che Aziz Ali, Abdullah Adli Zakaria, Mohd Shahimi Sali
Format: Article
Language:English
Published: SpringerOpen 2018-12-01
Series:Journal of Petroleum Exploration and Production Technology
Subjects:
Online Access:http://link.springer.com/article/10.1007/s13202-018-0591-8
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spelling doaj-3a52f59a1a074497a45e3ec13ce0cc012020-11-24T21:57:28ZengSpringerOpenJournal of Petroleum Exploration and Production Technology2190-05582190-05662018-12-01931593161410.1007/s13202-018-0591-8An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospectEkundayo Joseph Adepehin0Che Aziz Ali1Abdullah Adli Zakaria2Mohd Shahimi Sali3Geology Program, Faculty of Science and Technology, Universiti Kebangsaan MalaysiaGeology Program, Faculty of Science and Technology, Universiti Kebangsaan MalaysiaResource Exploration, Malaysia Petroleum Management, PETRONASResource Exploration, Malaysia Petroleum Management, PETRONASAbstract An overview and integration of key petroleum exploration findings in the onshore Central Sarawak Basin, NW Borneo in the last 2 decades is presented. Findings revealed that critical moments for the generation and preservation of hydrocarbon may be found in the Early Oligocene, Early Miocene, and Late Miocene times. Geochemical data of ninety-five (95) source rocks suggest TOC values of 1.54 wt% (Miri Formation) to 70.00 wt% (Nyalau Formation) with promising S 2 and S 2/S 3 ratios. T Max fell below the 435 °C maturation threshold. Reservoir facies of the Nyalau, Belait, and Lambir formations and their subsurface equivalents have moderate-to-poor poro-perm properties. Reservoir plays in the area are the Oligocene–Miocene clastics and limestones of Cycles I, II, III, and IV. Significant diagenetic modification is evident in analogue reservoir sandstones, and could constitute major poro-perm control in subsurface reservoir units. Observed predominance of structural related traps gleaned from seismic data is a reflection of the paleotectonic (Sarawak orogenic) event (ca. 40 − 36 Ma) associated with the region. Shale rocks overlying possible reservoirs and observed juxtaposition of reservoir units against impermeable beds provide seal integrity. Deeply seated faults are potential conduits, in addition to buoyancy. Concentration of future research efforts on petroleum/basin modeling and subsurface reservoir assessment was to further improve current understanding of the under-explored onshore Central Sarawak.http://link.springer.com/article/10.1007/s13202-018-0591-8Onshore Sarawak BasinBalingian ProvinceTinjar ProvincePetroleum systemSource rocksReservoir rocks
collection DOAJ
language English
format Article
sources DOAJ
author Ekundayo Joseph Adepehin
Che Aziz Ali
Abdullah Adli Zakaria
Mohd Shahimi Sali
spellingShingle Ekundayo Joseph Adepehin
Che Aziz Ali
Abdullah Adli Zakaria
Mohd Shahimi Sali
An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospect
Journal of Petroleum Exploration and Production Technology
Onshore Sarawak Basin
Balingian Province
Tinjar Province
Petroleum system
Source rocks
Reservoir rocks
author_facet Ekundayo Joseph Adepehin
Che Aziz Ali
Abdullah Adli Zakaria
Mohd Shahimi Sali
author_sort Ekundayo Joseph Adepehin
title An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospect
title_short An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospect
title_full An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospect
title_fullStr An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospect
title_full_unstemmed An overview of 20 years’ hydrocarbon exploration studies and findings in the Late Cretaceous-to-Tertiary onshore Central Sarawak, NW Borneo: 1997–2017 in retrospect
title_sort overview of 20 years’ hydrocarbon exploration studies and findings in the late cretaceous-to-tertiary onshore central sarawak, nw borneo: 1997–2017 in retrospect
publisher SpringerOpen
series Journal of Petroleum Exploration and Production Technology
issn 2190-0558
2190-0566
publishDate 2018-12-01
description Abstract An overview and integration of key petroleum exploration findings in the onshore Central Sarawak Basin, NW Borneo in the last 2 decades is presented. Findings revealed that critical moments for the generation and preservation of hydrocarbon may be found in the Early Oligocene, Early Miocene, and Late Miocene times. Geochemical data of ninety-five (95) source rocks suggest TOC values of 1.54 wt% (Miri Formation) to 70.00 wt% (Nyalau Formation) with promising S 2 and S 2/S 3 ratios. T Max fell below the 435 °C maturation threshold. Reservoir facies of the Nyalau, Belait, and Lambir formations and their subsurface equivalents have moderate-to-poor poro-perm properties. Reservoir plays in the area are the Oligocene–Miocene clastics and limestones of Cycles I, II, III, and IV. Significant diagenetic modification is evident in analogue reservoir sandstones, and could constitute major poro-perm control in subsurface reservoir units. Observed predominance of structural related traps gleaned from seismic data is a reflection of the paleotectonic (Sarawak orogenic) event (ca. 40 − 36 Ma) associated with the region. Shale rocks overlying possible reservoirs and observed juxtaposition of reservoir units against impermeable beds provide seal integrity. Deeply seated faults are potential conduits, in addition to buoyancy. Concentration of future research efforts on petroleum/basin modeling and subsurface reservoir assessment was to further improve current understanding of the under-explored onshore Central Sarawak.
topic Onshore Sarawak Basin
Balingian Province
Tinjar Province
Petroleum system
Source rocks
Reservoir rocks
url http://link.springer.com/article/10.1007/s13202-018-0591-8
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