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Bojongmanik Formation Sedimentation Mechanism in the Middle to Late Miocene (N9-N17) in the Rangkasbitung Basin

Scientific Contributions Oil and Gas · Vol. 43 No. 3 (2020) · hlm. 115–123

DOI
10.29017/SCOG.43.3.551
ISSN
2541-0520, 2089-3361
Terbit
2020-12-30
Penerbit
Testing Center for Oil and Gas LEMIGAS
Bahasa
eng
Lisensi
creativecommons.org/licenses/by/4.0

Abstrak

The Rangkasbitung Basin, is a part of Banten Depression which was formed by a normal fault, and then fi lled by marine deposits. This research carried out to understand the sedimentation process of Middle Miocene Bojongmanik deposits, the age, paleoenvironment and lithology (sediment sequence). In this research, 55 samples were taken from the study area, approximately 595 km2. Measurement of the stratigraphic section is carried out to determine the correlation both vertically and horizontally. The residue of dissolving peroxide method was carried out during the samples preparation. Then genus and species of planktonic and benthonic foraminifera were identifi ed and determined. The foraminifera analysis guide has been used to determine the age and depositional environment. The sequences of Bojongmanik Formation were deposited in Middle to Upper Miocene (N9 to N17). Based on the planktonic foraminifera distribution, the succession of each sequence can be correlated. During Middle Miocene (N9 - N12), the lowest part of Bojongmanik Formation is deposited at 100m-200m and 100m-80m depth, while in the other site, the correlated sequence is recorded that deposited at 80m-20m depth (outer to edge of inner neritic facies). In late Middle Miocene (N13 - N14), the regression process was happened. Almost the succession was deposited on land, while in deep site, a less part of sediments was formed as land facies but the most of it deposited as marine facies. In Upper Miocene (N 15 - N 17), the sedimentation continued in the transitional to edge neritic in back mangrove to mangrove environmental setting (upper to lower delta plain), and in other sites the sediment is no longer formed. Based on distribution of benthonic foraminifera there are observed the biofacies changes laterally. In bathymetric of depositional environment maps it can be depicted two higher paleoenvironmental sites (Cigudeg and Muncang highs) and two lower sites (Leuwiliang and Jasinga basins).

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  • Pusat Sumber Daya Mineral Batubara dan Panas Bumi
  • Bandung Institute of Technology
  • Universitas Sumatera Utara
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Rekan penulisOrganisasiArtikel bersama
Emi SukiyahAfiliasi tidak diketahui3
Adjat SudradjatAfiliasi tidak diketahui2
Rizki Satria RachmanPusat Sumber Daya Mineral Batubara dan Panas Bumi1
Martha Magdalena NanlohyAfiliasi tidak diketahui1
Fery ErawanAfiliasi tidak diketahui1
Yudo AnggoroBandung Institute of Technology1
Prana Ugiana GioUniversitas Sumatera Utara1
Rezzy Eko CarakaAfiliasi tidak diketahui1
Anjar Dimara SaktiAfiliasi tidak diketahui1
Bens PardameanAfiliasi tidak diketahui1
Muhammad Khahfi ZuhandaAfiliasi tidak diketahui1
Khairunnisa SupardiAfiliasi tidak diketahui1
Rung Ching ChenAfiliasi tidak diketahui1
Noor Ell GoldameirAfiliasi tidak diketahui1
Avia Enggar TyastiAfiliasi tidak diketahui1
Rumanintya Lisaria PutriAfiliasi tidak diketahui1
Amos LukasAfiliasi tidak diketahui1
Rishan AdhaAfiliasi tidak diketahui1
Pahrudin PahrudinAfiliasi tidak diketahui1
Fahmi Ali HudaefiAfiliasi tidak diketahui1

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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">Bojongmanik Formation Sedimentation Mechanism in the Middle to Late Miocene (N9-N17) in the Rangkasbitung Basin</dc:title>
	<dc:creator xml:lang="en">Syahrulyati, Tety</dc:creator>
	<dc:creator xml:lang="en">Isnaniawardhani, Vijaya</dc:creator>
	<dc:creator xml:lang="en">Rosana, Mega Fattima</dc:creator>
	<dc:creator xml:lang="en">Winantris, Winantris</dc:creator>
	<dc:subject xml:lang="en">Sedimentation mechanism</dc:subject>
	<dc:subject xml:lang="en">Bojongmanik formation</dc:subject>
	<dc:subject xml:lang="en">Rangkasbitung basin</dc:subject>
	<dc:description xml:lang="en">The Rangkasbitung Basin, is a part of Banten Depression which was formed by a normal fault, and then fi lled by marine deposits. This research carried out to understand the sedimentation process of Middle Miocene Bojongmanik deposits, the age, paleoenvironment and lithology (sediment sequence). In this research, 55 samples were taken from the study area, approximately 595 km2. Measurement of the stratigraphic section is carried out to determine the correlation both vertically and horizontally. The residue of dissolving peroxide method was carried out during the samples preparation. Then genus and species of planktonic and benthonic foraminifera were identifi ed and determined. The foraminifera analysis guide has been used to determine the age and depositional environment. The sequences of Bojongmanik Formation were deposited in Middle to Upper Miocene (N9 to N17). Based on the planktonic foraminifera distribution, the succession of each sequence can be correlated. During Middle Miocene (N9 - N12), the lowest part of Bojongmanik Formation is deposited at 100m-200m and 100m-80m depth, while in the other site, the correlated sequence is recorded that deposited at 80m-20m depth (outer to edge of inner neritic facies). In late Middle Miocene (N13 - N14), the regression process was happened. Almost the succession was deposited on land, while in deep site, a less part of sediments was formed as land facies but the most of it deposited as marine facies. In Upper Miocene (N 15 - N 17), the sedimentation continued in the transitional to edge neritic in back mangrove to mangrove environmental setting (upper to lower delta plain), and in other sites the sediment is no longer formed. Based on distribution of benthonic foraminifera there are observed the biofacies changes laterally. In bathymetric of depositional environment maps it can be depicted two higher paleoenvironmental sites (Cigudeg and Muncang highs) and two lower sites (Leuwiliang and Jasinga basins).</dc:description>
	<dc:publisher xml:lang="en">Testing Center for Oil and Gas LEMIGAS</dc:publisher>
	<dc:date>2020-12-30</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/551</dc:identifier>
	<dc:identifier>10.29017/SCOG.43.3.551</dc:identifier>
	<dc:source xml:lang="en">Scientific Contributions Oil and Gas; Vol. 43 No. 3 (2020); 115-123</dc:source>
	<dc:source xml:lang="id">Scientific Contributions Oil and Gas; Vol 43 No 3 (2020); 115-123</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/551/314</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2020 © Copyright by Authors. Published by LEMIGAS</dc:rights>
	<dc:rights xml:lang="en">https://creativecommons.org/licenses/by/4.0</dc:rights>
</oai_dc:dc>