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Contact Name
Minarwan
Contact Email
minarwanx@gmail.com
Phone
+6281908602813
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bs.fosi@gmail.com
Editorial Address
Forum Sedimentologiwan Indonesia (FOSI) Komisi Sedimentologi Ikatan Ahli Geologi Indonesia (IAGI) Jl. Ciledug Raya Kav. 109 Cipulir, Kebayoran Lama, Jakarta Selatan, Indonesia
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Kota adm. jakarta selatan,
Dki jakarta
INDONESIA
Berita Sedimentologi
ISSN : 08539413     EISSN : 2807274X     DOI : https://doi.org/10.51835/bsed
Core Subject : Science,
BERITA SEDIMENTOLOGI aims to disseminate knowledge on the field of sedimentary geology to its readers. The journal welcomes contributions in the form of original research articles, review articles, short communications and discussions and replies. Occasionally, Berita Sedimentologi also includes field trip reports and book reviews, which are published only after going through peer-review processes. The main geographical areas of interest are Indonesia and SE Asia, however contribution from the rest of the world is also welcome. Berita Sedimentologi covers broad topics within sedimentary geology, particularly on depositional processes and their records in the rocks, petrology, sedimentology and stratigraphy of both siliciclastic and carbonate rocks; sequence stratigraphy, paleontology, biostratigraphy and sedimentary geochemistry. The journal also accepts articles on interdisciplinary research in sedimentary basin analysis, including large-scale basin geodynamics processes, mechanism of sedimentary basin formation, earth surface processes, sediment routing systems, petroleum geoscience and applied sedimentary geology analysis for mining and engineering geology.
Articles 10 Documents
Search results for , issue "Vol 23, No 1 (2012)" : 10 Documents clear
Middle Jurassic Ammonites from The Cendrawasih Bay Coast and North Lengguru Fold-Belt, West PApua: Implications of a ‘Forgotten’ 1913 Paper van Gorsel, J.T. (Han)
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1328.411 KB) | DOI: 10.51835/bsed.2012.23.1.191

Abstract

Occurrences of Middle Jurassic bathyal shales with typical ammonite faunas were reported from the 'Birds Neck', West Papua, in 1913 and 1927 publications but these appear to be largely forgotten. They signify an eastern limit for the gas-productive Middle Jurassic sands of Bintuni Bay and thus have significant negative implications for the potential of Mesozoic hydrocarbon plays in Cenderawasih Bay.
Book Review: Biodiversity, Biogeography and Nature Conservation in Wallacea and New Guinea (Volume 1) Darman, Herman
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1298.415 KB) | DOI: 10.51835/bsed.2012.23.1.196

Abstract

Biodiversity, Biogeography and Nature Conservation in Wallacea and New Guinea (Volume 1)Edited byDmitry Telnov, Ph.D.Chairman of Coleopterology, The Entomological Society of Latvia Stopinunovads, Darzaiela 10, DZIDRINAS, LV-2130, Latvia / Lettland / LettonieWebsites: http://leb.daba.lv and http://www.zin.ru/Animalia/Coleoptera/eng/telnov.htm
Tectonic and Regional Structure of Seram and the Banda Arc Hill, Kevin C.
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2258.593 KB) | DOI: 10.51835/bsed.2012.23.1.187

Abstract

Seram and the Banda Sea lie between the passive margin tectonics of Australia’s Northwest Shelf and the active margin tectonics of New Guinea, both of which have played an important role in the structure, facies distribution and hydrocarbon prospectivity of the area.A restored cross section across Seram and a 3D model reconstruction of the Miocene evolution of the Banda Arc reveal the history of the area. The Proto-Banda Sea is considered to have formed in the Permian, including a marginal basin with Permian oceanic crust. Extension was terminated by Triassic orogenesis in New Guinea supplying vast amounts of Triassic detritus (Kanikeh) to the stretched Banda margins. In the Late Triassic, the sediment supply was diminished in part due to the renewed onset of extension along the New Guinea margin. It is notable that the Triassic orogeny was very similar to the Miocene to Recent orogeny in New Guinea. As Triassic sediment supply was reduced, carbonate banks were locally built up (Manusela reservoir) surrounded by starved source rock facies. The margin subsided in the Jurassic and was starved of sediment until the Tertiary when renewed tectonic activity in New Guinea supplied distal carbonates and marls, mainly in the Miocene. Around 10 Ma, the Indonesian Arc impinged on the Permian oceanic lithosphere of the Proto Banda Sea, which was then rapidly subducted, sinking under its own weight. The Arc advanced rapidly eastwards towards Timor and Seram, generating a collisional margin in Timor, but a strongly transpressional margin in Seram. The first phase of collision in Seram at ~6 Ma involved overthrusting of an accretionary prism, largely comprising Kanikeh sediments, but also some oceanic fragments. The second phase of orogenesis in Seram involved thrusting of the continental margin beneath the overthrust, creating highly fractured antiformal stacks in the Manusela encased in Kanikeh seal and source rocks, as in the Oseil oilfield. To the east an imbricate thrust zone has formed in the Cretaceous and Tertiary sequences which is now impinging on the Misool-Onin Arch.
Interplay between Submarine Depositional Processes and Recent Tectonics in the Biak Basin, Western Papua, Eastern Indonesia Bertoni, Claudia; Álvarez, Juan
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1333.36 KB) | DOI: 10.51835/bsed.2012.23.1.192

Abstract

The offshore Biak Basin between Biak and Yapen Islands is a transtensional pull-apart basin. Deposition along basin margins is strongly influenced by active faulting. The bathymetric map of the basin shows submarine depositional processes occurred during relatively recent tectonic activity.
Origins of the Banda Arcs Collisional Orogen and the Banda Sea Satyana, Awang Harun
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (849.792 KB) | DOI: 10.51835/bsed.2012.23.1.188

Abstract

Many of the best examples of young arc-continent collision are found in eastern Indonesia, where the northern margin of Australia has been in collision throughout the Neogene with a succession of island arc systems. The Banda Arc is the youngest of these collision zones and forms the present plate boundary in this region. Behind the Banda Arcs, is the Banda Sea oceanic crust with its debatable origin.
Seismic to Geological Modeling Workflow, an Integrated Approache to Determine the Reservoir Quality of a Fractured Limestone: Oseil Field Example Lapulisa, Arie K.; Andrianto, Roy; Dradjat, Anggoro S.
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1767.911 KB) | DOI: 10.51835/bsed.2012.23.1.193

Abstract

Natural fractured carbonate reservoir is extremely challenging in terms of reservoir characterization due to its high heterogeneity of reservoir property and also of its low oil recoveries. This paper will show how the integration of seismic data and well data had helped significantly for the well placement and also in the well completion stage.The datasets that are available and being used in this process are 3D seismic, seismic Inversion, seismic attributes, conventional log and borehole image log. All these data are being utilized in an integrated way to characterize the fractures behavior of the reservoir.
New Insights into the Geological Evolution of Eastern Indonesia from Recent Research Projects by the SE Asia Research Group Watkinson, Ian M.; Hall, Robert; Cottam, Mike A.; Sevastjanova, Inga; Suggate, Simon; Gunawan, Indra; Pownall, Jonathan M.; Hennig, Juliane; Ferdian, Farid; Gold, David; Zimmermann, Sebastian; Rudyawan, Alfend; Advocaat, Eldert
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1328.003 KB) | DOI: 10.51835/bsed.2012.23.1.189

Abstract

Eastern Indonesia has a prolonged, complex tectonic history. It is where the Eurasian, Indo-Australian, Caroline and Philippine Sea plates converge, and where processes such as subduction, obduction, slab rollback, rifting, supracrustal extension, lower crustal flow and exhumation are very young or still active.For these reasons, the SE Asia Research Group (SEARG) at Royal Holloway, University of London, has made Eastern Indonesia one of its major research themes in recent years. The SEARG has been conducting geological research in SE Asia since 1982. Work has been undertaken in Indonesia, Malaysia, Thailand, the Philippines, Vietnam and the South China Sea. In 2012 the SEARG is directed by Professor Robert Hall, and involves 12 postgraduate students, 2 postdoctoral researchers, a large number of academic staff, research associates and collaborators in the UK and overseas. The group is funded by a consortium of oil companies.Here we summarise recent and ongoing SEARG projects in Eastern Indonesia. Most of the projects are field-based, but they all also employ new data and techniques, such as 40Ar-39Ar, U-Pb dating (SHRIMP and LA-ICP-MS), Hf isotope dating (LA-MC-ICP-MS), UTh/ He dating, multibeam bathymetry, high quality seismic and remote sensing data.
A Guest Lecture and An AAPG Course at Sultan Hasanuddin University, Makassar, Indonesia Reijers, Tom J.A.
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (803.222 KB) | DOI: 10.51835/bsed.2012.23.1.194

Abstract

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Seismic Expression of Geological Features in Seram Sea: Seram Trough, Misool-Onin Ridge and Sedimentary Basin Darman, Herman; Reemst, Paul
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2437.186 KB) | DOI: 10.51835/bsed.2012.23.1.190

Abstract

The Seram Sea is located between Seram Island and the Bird’s Head of Papua, Eastern Indonesia. This sea extends to the east towards Bintuni Bay. Some part of the sea, between Seram and Misool are deeper than 2000 m. The Seram Island is mountainous with altitudes reaching 3000 m above sea level at the center of the island.Several seismic surveys have been conducted to understand the geology of this region. The first seismic sections were published by Hamilton in 1979. These seismic sections were acquired by Western Geophysical for Phillips Petroleum. In 2000, Schlumberger published some seismic lines acquired in 1997 with an improved resolution improvement. More higher quality seismic lines were acquired as part of non exclusive and multi-client projects in the late 1990’s which provide a better geological understanding of the region and lead to several petroleum exploration opportunities.This article discusses the seismic expression of several geological features in the Seram Sea vicinity based on published seismic sections. The offshore seismic sections cover part of the imbricated complex in the north of Seram Island, the Seram Trough, the Misool-Onin High and the sedimentary basins the east of the Misool-Onin Ridge, such as the Tamaloi-Malagot Basin, the Semai-Berau Basin and the Bintuni Basin.
Book Review: The SE Asian Gateway: History and Tectonic of the Australia-Asia Collision Reijers, Tom J.A
Berita Sedimentologi Vol 23, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (331.233 KB) | DOI: 10.51835/bsed.2012.23.1.195

Abstract

The SE Asian Gateway: History and Tectonic of the Australia-Asia CollisionEdited by R. Hall, M. A. Cottam and M. E. J. WilsonGeological Society, London, Special Publication, 355, 2011, 381 pp. ISBN 978-1-86239-329-5.

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