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Mapping Iron Oxide Distribution on the Ground Surface of the Tugu Barat Oil and Gas Field Using Landsat 8 OLI and Field Data

Scientific Contributions Oil and Gas · Vol. 47 No. 3 (2024) · hlm. 189–203

DOI
10.29017/SCOG.47.3.1634
ISSN
2541-0520, 2089-3361
Terbit
2024-12-01
Penerbit
Testing Center for Oil and Gas LEMIGAS
Bahasa
eng
Lisensi
creativecommons.org/licenses/by/4.0

Abstrak

Previous studies have demonstrated that Landsat series data can be utilized to map rock change in arid and semi-arid environments. In this study, Landsat 8 Operational Land Imager (OLI) was used to map the presence of iron oxide (ferrous, ferric, and hematite) in the topsoil of the Tugu Barat Oil and Gas Field, Northwest Java Basin, Indonesia. The aim is to map the distribution of iron oxide and analyze it for detection of the presence of microseepage. The results show that the concentration of the mineral hematite indicates an anomaly, where the edge of the field is very low and tends to rise in the middle, but this condition is unclear, because of the presence of red soil containing high hematite in the north. Based on analysis indicates an anomaly, where the edge of the field is very low and tends to rise in the middle, but this condition is unclear, because of the presence of red soil containing high hematite in the north. Based on analysis of Landsat 8 OLI data, ferrous oxide concentrations show an increase at the edge of the field, especially in the southeast. However, this condition is less visible in the west because of the high vegetation density. The ferric oxide concentration shows the opposite pattern to the ferrous oxide concentration. These results are supported by the ferrous oxide index results from soil reflectance spectra recorded using Analytical Spectral Devices (ASD). Where the ferrous oxide concentration is low at the edge then tends to rise in the middle of the field. Meanwhile, the analysis of ferric oxide from the spectral reflectance of soil from ASD results does not show clear differences. The Normalized Iron Oxide Difference Index (NIODI) analysis shows the presence of small amounts of hematite and no geotite. The research results show evidence of microseepage indications at the edge of the field, especially at the southeastern edge. Iron oxide mapping has the potential to support oil and gas exploration through analysis of alteration processes which are thought to be the impact of micro-seepage.

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  • Bandung Institute of Technology
  • National Research and Innovation Agency
  • Lampung University
  • Indonesian National Institute of Aeronautics and Space
  • Udayana University
  • IPB University
  • Andalas University
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Rekan penulisOrganisasiArtikel bersama
Bambang WidarsonoNational Research and Innovation Agency11
Deni SuwardhiBandung Institute of Technology7
Rian NurtyawanBandung Institute of Technology6
Mohamad RomliNational Research and Innovation Agency6
Diana DwiyanartiNational Research and Innovation Agency6
Mochamad Firman GhazaliLampung University5
Fenny Martha DwivanyBandung Institute of Technology4
Riantini VirtrianaBandung Institute of Technology4
Djoko SunarjantoNational Research and Innovation Agency4
Soni DarmawanBandung Institute of Technology3
Dudung Muhally HakimBandung Institute of Technology3
I Wayan NuarsaUdayana University3
Shafarina Wahyu TrisyantiBandung Institute of Technology3
I NyomanUdayana University2
Agus SutantoAndalas University2
Husna NugrahaprajaBandung Institute of Technology2
Ishak Hanafiah IsmullahBandung Institute of Technology2
Luisa Febrina AmaloIPB University1
Rahmat HidayatIPB University1
Anggun TridawatiBandung Institute of Technology1
Mamad SugandiLampung University1
Aqilla Fitdhea AnestaLampung University1
Laode M Golok JayaAfiliasi tidak diketahui1
Armi SusandiBandung Institute of Technology1
Katmoko Ari SambodoIndonesian National Institute of Aeronautics and Space1
M. Angga Hadi PratamaAfiliasi tidak diketahui1
Hasan Adi NugrahaBandung Institute of Technology1
Anjar Dimara SaktiBandung Institute of Technology1
Muhammad Alsamtu Tita Sabila Pratama SuhartonoAkita University1

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Sumber metadata: OAI-PMH (metadata jurnal) https://journal.lemigas.esdm.go.id/index.php/SCOG/oai, pertama di-harvest 10 Nov 2026, terakhir terlihat 10 Nov 2026.
Metadata asli (oai_dc)
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	<dc:title xml:lang="en">Mapping Iron Oxide Distribution on the Ground Surface of the Tugu Barat Oil and Gas Field Using Landsat 8 OLI and Field Data</dc:title>
	<dc:creator xml:lang="en">Susantoro, Tri Muji</dc:creator>
	<dc:creator xml:lang="en">Suliantara, Suliantara</dc:creator>
	<dc:creator xml:lang="en">Wikantika, Ketut</dc:creator>
	<dc:creator xml:lang="en">Saepuloh, Asep</dc:creator>
	<dc:creator xml:lang="en">Harto, Agung Budi</dc:creator>
	<dc:creator xml:lang="en">Setiawan, Herru Lastiadi</dc:creator>
	<dc:creator xml:lang="en">Agustin, Fitriani</dc:creator>
	<dc:creator xml:lang="en">Jayati, Adis</dc:creator>
	<dc:creator xml:lang="en">Kurdianto, Kurdianto</dc:creator>
	<dc:creator xml:lang="en">Sulma, Sayidah</dc:creator>
	<dc:creator xml:lang="en">Sukristiyanti, Sukristiyanti</dc:creator>
	<dc:subject xml:lang="en">iron oxide</dc:subject>
	<dc:subject xml:lang="en">soil spectral</dc:subject>
	<dc:subject xml:lang="en">hematite</dc:subject>
	<dc:subject xml:lang="en">NIODI</dc:subject>
	<dc:subject xml:lang="en">landsat 8 OLI</dc:subject>
	<dc:description xml:lang="en">Previous studies have demonstrated that Landsat series data can be utilized to map rock change in arid and semi-arid environments. In this study, Landsat 8 Operational Land Imager (OLI) was used to map the presence of iron oxide (ferrous, ferric, and hematite) in the topsoil of the Tugu Barat Oil and Gas Field, Northwest Java Basin, Indonesia. The aim is to map the distribution of iron oxide and analyze it for detection of the presence of microseepage. The results show that the concentration of the mineral hematite indicates an anomaly, where the edge of the field is very low and tends to rise in the middle, but this condition is unclear, because of the presence of red soil containing high hematite in the north. Based on analysis indicates an anomaly, where the edge of the field is very low and tends to rise in the middle, but this condition is unclear, because of the presence of red soil containing high hematite in the north. Based on analysis of Landsat 8 OLI data, ferrous oxide concentrations show an increase at the edge of the field, especially in the southeast. However, this condition is less visible in the west because of the high vegetation density. The ferric oxide concentration shows the opposite pattern to the ferrous oxide concentration. These results are supported by the ferrous oxide index results from soil reflectance spectra recorded using Analytical Spectral Devices (ASD). Where the ferrous oxide concentration is low at the edge then tends to rise in the middle of the field. Meanwhile, the analysis of ferric oxide from the spectral reflectance of soil from ASD results does not show clear differences. The Normalized Iron Oxide Difference Index (NIODI) analysis shows the presence of small amounts of hematite and no geotite. The research results show evidence of microseepage indications at the edge of the field, especially at the southeastern edge. Iron oxide mapping has the potential to support oil and gas exploration through analysis of alteration processes which are thought to be the impact of micro-seepage.</dc:description>
	<dc:publisher xml:lang="en">Testing Center for Oil and Gas LEMIGAS</dc:publisher>
	<dc:date>2024-12-01</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.lemigas.esdm.go.id/index.php/SCOG/article/view/1634</dc:identifier>
	<dc:identifier>10.29017/SCOG.47.3.1634</dc:identifier>
	<dc:source xml:lang="en">Scientific Contributions Oil and Gas; Vol. 47 No. 3 (2024); 189-203</dc:source>
	<dc:source xml:lang="id">Scientific Contributions Oil and Gas; Vol 47 No 3 (2024); 189-203</dc:source>
	<dc:source>2541-0520</dc:source>
	<dc:source>2089-3361</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://journal.lemigas.esdm.go.id/index.php/SCOG/article/view/1634/pdf</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2024 © Copyright by Authors. Published by LEMIGAS</dc:rights>
	<dc:rights xml:lang="en">https://creativecommons.org/licenses/by/4.0</dc:rights>
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