Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality

An integrated study of several methods to characterize a carbonate reservoir provides a comprehensive result on carbonate facies and diagenesis. Therefore, a study on the Tertiary carbonate reservoir at the East Arm of Sulawesi area, Banggai – Sula Basin, is intended to determine the Salodik Group c...

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Published in:Indonesian Journal on Geoscience
Main Authors: Jambak, Moeh. Ali, Ibrahim, Ivan, Harnest, Billy, Irano, Teddy, Prabawa, Gusti, Luthfi, Ramadhan, Prasetyo, Ardyand Budi
Format: Article in Journal/Newspaper
Language:English
Published: Geological Agency 2024
Subjects:
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/811
https://doi.org/10.17014/ijog.11.1.91-109
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author Jambak, Moeh. Ali
Ibrahim, Ivan
Harnest, Billy
Irano, Teddy
Prabawa, Gusti
Luthfi, Ramadhan
Prasetyo, Ardyand Budi
author_facet Jambak, Moeh. Ali
Ibrahim, Ivan
Harnest, Billy
Irano, Teddy
Prabawa, Gusti
Luthfi, Ramadhan
Prasetyo, Ardyand Budi
author_sort Jambak, Moeh. Ali
collection Indonesian Journal on Geoscience
container_issue 1
container_start_page 91
container_title Indonesian Journal on Geoscience
container_volume 11
description An integrated study of several methods to characterize a carbonate reservoir provides a comprehensive result on carbonate facies and diagenesis. Therefore, a study on the Tertiary carbonate reservoir at the East Arm of Sulawesi area, Banggai – Sula Basin, is intended to determine the Salodik Group carbonate reservoir facies and diagenesis. Moreover, the purpose of this study is to determine the intensity and implication of syn-depositional or post-depositional processes, and to provide the reservoir final properties values, such as porosity and permeability to classify the reservoir quality. The methods of the study are based on carbonate fieldwork mapping to obtain samples on distributed traverses. Further analyses are the laboratory works to determine facies and diagenesis features on a more detailed scale. This study shows several facies, dominantly classified into reefal packstone, planktonic foraminifera packstone-wackestone, large foram packstone-mudstone, skeletal packstone-wackestone, planktonic-large foraminifera packstone-wackestone, and large foraminifera-red algae packstone. The dominant diagenesis processes are cementation and dissolution. Moreover, meteoric vadose and meteoric phreatic are predominantly the main diagenesis environment of Salodik Group formations. Furthermore, the dominant diagenesis stage is Eogenetic. The post-depositional process or the diagenetic processes, provides a more significant impact on carbonate reservoir properties than the syn-depositional process as shown on lithofacies texture. However, in general, from the younger to the oldest formation of Salodik Group, this shows a decreasing trend of reservoir properties due to the dominantcementation process in the oldest formation. Overall, the reservoir quality referring to porosity value is classified as negligible to excellent. While, based on permeability data, it is classified as the tight to good reservoir.
format Article in Journal/Newspaper
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
geographic East Arm
geographic_facet East Arm
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op_doi https://doi.org/10.17014/ijog.11.1.91-109
op_relation https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/811/463
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op_rights Copyright (c) 2024 Indonesian Journal on Geoscience
op_source Indonesian Journal on Geoscience; Vol. 11 No. 1 (2024); 91-109
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spelling ftjijog:oai:ojs.pkp.sfu.ca:article/811 2025-06-08T14:06:30+00:00 Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality Jambak, Moeh. Ali Ibrahim, Ivan Harnest, Billy Irano, Teddy Prabawa, Gusti Luthfi, Ramadhan Prasetyo, Ardyand Budi 2024-05-17 application/pdf https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/811 https://doi.org/10.17014/ijog.11.1.91-109 eng eng Geological Agency https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/811/463 https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/811 Copyright (c) 2024 Indonesian Journal on Geoscience Indonesian Journal on Geoscience; Vol. 11 No. 1 (2024); 91-109 2355-9306 2355-9314 Carbonate reservoir Salodik Group carbonate facies diagenesis porosity permeability reservoir quality info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 2024 ftjijog https://doi.org/10.17014/ijog.11.1.91-109 2025-05-09T11:20:21Z An integrated study of several methods to characterize a carbonate reservoir provides a comprehensive result on carbonate facies and diagenesis. Therefore, a study on the Tertiary carbonate reservoir at the East Arm of Sulawesi area, Banggai – Sula Basin, is intended to determine the Salodik Group carbonate reservoir facies and diagenesis. Moreover, the purpose of this study is to determine the intensity and implication of syn-depositional or post-depositional processes, and to provide the reservoir final properties values, such as porosity and permeability to classify the reservoir quality. The methods of the study are based on carbonate fieldwork mapping to obtain samples on distributed traverses. Further analyses are the laboratory works to determine facies and diagenesis features on a more detailed scale. This study shows several facies, dominantly classified into reefal packstone, planktonic foraminifera packstone-wackestone, large foram packstone-mudstone, skeletal packstone-wackestone, planktonic-large foraminifera packstone-wackestone, and large foraminifera-red algae packstone. The dominant diagenesis processes are cementation and dissolution. Moreover, meteoric vadose and meteoric phreatic are predominantly the main diagenesis environment of Salodik Group formations. Furthermore, the dominant diagenesis stage is Eogenetic. The post-depositional process or the diagenetic processes, provides a more significant impact on carbonate reservoir properties than the syn-depositional process as shown on lithofacies texture. However, in general, from the younger to the oldest formation of Salodik Group, this shows a decreasing trend of reservoir properties due to the dominantcementation process in the oldest formation. Overall, the reservoir quality referring to porosity value is classified as negligible to excellent. While, based on permeability data, it is classified as the tight to good reservoir. Article in Journal/Newspaper Planktonic foraminifera Indonesian Journal on Geoscience East Arm ENVELOPE(62.875,62.875,-67.600,-67.600) Indonesian Journal on Geoscience 11 1 91 109
spellingShingle Carbonate reservoir
Salodik Group
carbonate facies
diagenesis
porosity
permeability
reservoir quality
Jambak, Moeh. Ali
Ibrahim, Ivan
Harnest, Billy
Irano, Teddy
Prabawa, Gusti
Luthfi, Ramadhan
Prasetyo, Ardyand Budi
Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality
title Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality
title_full Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality
title_fullStr Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality
title_full_unstemmed Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality
title_short Reinterpretation of Salodik Group Performance Based on Facies and Diagenesis Approaches to Classify Reservoir Quality
title_sort reinterpretation of salodik group performance based on facies and diagenesis approaches to classify reservoir quality
topic Carbonate reservoir
Salodik Group
carbonate facies
diagenesis
porosity
permeability
reservoir quality
topic_facet Carbonate reservoir
Salodik Group
carbonate facies
diagenesis
porosity
permeability
reservoir quality
url https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/811
https://doi.org/10.17014/ijog.11.1.91-109