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Berita Sedimentologi
Published by Forum Sedimentologiwan Indonesia
ISSN : 08539413     EISSN : 2807274X     DOI : https://doi.org/10.51835/bsed
Core Subject : Science,
Earth & Planetary Sciences
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.
Arjuna Subject : Ilmu Bumi dan Planet (semua kategori) - Geologi
Articles 7 Documents
 1 
Search results for , issue "Vol 10, No 1 (1998)" : 7 Documents clear
Depositional and Diagenetic Models of Miocene Parigi and Pre-Parigi Carbonates Offshore Northwest Java, Indonesia Fransiskus J. Sugiaman
Berita Sedimentologi Vol 10, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1100.133 KB) | DOI: 10.51835/bsed.1998.10.1.275

Abstract

An integrated approach to understanding the deposition and diagenesis of the Parigi carbonates in KL area and the Pre-Parigi carbonates in APN area has been developed using petrographic, well logs and seismic analysis.
The Effects of Eustatic Sea Level Change in the Development of Carbonate Reservoir: An Overview Herman Darman
Berita Sedimentologi Vol 10, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (4446.24 KB) | DOI: 10.51835/bsed.1998.10.1.276

Abstract

There are some major factors that control the variations in stratal patterns and lithofacies distributions within carbonate rocks. They include tectonic subsidence, eustatic change of sea-level, sediment volume, and climate. However, the major control over carbonate sedimentations is the eustatic change of sea-level.The cyclic changes in global sea level produce reciprocal sedimentations that alternately open and shut off transport of terrigenous clastics across the shelf into the basain. These clastics are highly involved in carbonate deposits development. During high stand of sea level, carbonates are the dominant lithologies that accumulates on the shelf, shelf margin, and in the basin. During succedingly lower stands of sea level, terrigenous clastics progrades across the shelf, and initial clastic sedimentation occures as they by-passes the slope and accumulates in the basin.Sea-level changes not only controls the carbonate sedimentation, but also controls the thickness and the internal structures of the carbonate rocks. Various depositional environments produce by the sea level changes cause the heterogeneity of carbonate reservoir. The sea level changes are highly related to the carbonate reservoir creation, therefore it is important to understand their relationship.
Control on Carbonate Sedimentation of Tacipi Formation, South Sulawesi, Indonesia N. Alit Ascaria
Berita Sedimentologi Vol 10, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (930.081 KB) | DOI: 10.51835/bsed.1998.10.1.277

Abstract

South Sulawesi is located in the centre of a complex tectonic region where Indo-Australian, Eurasian and Paific plates interact and collide. The Tacipi Formation was deposited during the middle Miocene to early Pliocene in an intra-arc or fore-arc setting. Facies distribution, diagenesis and hydrocarbon potential of these carbonate was strongly influenced by the tectonostratigraphic setting, faulting, subsidence and relative sea level changes.
Probing the Third Dimension of the Reef Complex at Kepulauan Seribu: A Proposal for Gathering Seismic Profiles and Cores of Holocene Sediments Berita Sedimentologi
Berita Sedimentologi Vol 10, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (618.229 KB) | DOI: 10.51835/bsed.1998.10.1.273

Abstract

Integrated Data Services, Louisiana State University, and PT. Geoservices jointly announce their program of shooting shallow, high-resolution seismic profiles and trying these profiles with cores across the Kepulauan Seribu reef complex in the West Java Sea. The surface sediments of Kepulauan Seribu, 50 kilometers north of Jakarta, have been mapped in considerable detail; in addition, a few cores have been taken in shallow water reef environment. However, no deep-water coring nor shallow seismic data has been gathered to investigate the evolution of this modern reef complex. In fact, Holocene reef facies here sit atop equivalent Miocene Reef facies which produce at the giant Bima Field.This research program will gather a series of seismic profiles and take several cores along these profiles. All representative environments of deposition will be sampled with these techniques, including shallow- and deep-water settings. Companies are asked to participate in this program by taking part in data collection, in the sharing of samples, and in the funding of operational costs. A final report by the principal investigators will be distributed to participant companies.
Devonian Carbonate of Telen River, East Kalimantan Fransiskus Sugiaman; Ludy Andria
Berita Sedimentologi Vol 10, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1449.298 KB) | DOI: 10.51835/bsed.1998.10.1.278

Abstract

BSc Thesis submitted to Bandung Institute of Technology, 1990In 1925, the Dutch Colonial Government sent a scientific expedition team to East Kalimantan, which was called "Midden Oost Borneo Expeditie" and led by H. Witkamp. The expedition collected rock samples from Telen River, a tributary of Mahakam River. In 1940, L. Rutten analyzed the rock samples and found Devonian fossils, which were known as the oldest fossils in western part of Indonesia. The fossils were found in a dark, crystalline limestone and Marks (1951) included the limestone into Danau facies. The existence and location of the limestone is often mentioned and cited by many geologist, such as Van Bemmelen (1949), Marks (1957), Sartono (1970), and Soejono (1988), since it is assumed as a classical stratigraphic location.The location of the Devonicn limestone had never been revisited since the Dutch expedition, due to its remote location and difficult accessibility. The distribution of the Devonian limestone and its stratigraphic correlation with other units were still a mystery. Noticing the limitation of the geological information on the Devonian limestone, the Association of Geology Students "GEA" from Bandung Institute of Technology (ITB) organized a scientific expedition, which is called Devonian Expedition 1989. Field work was conducted in October to November 1989.
Carbonate Slope Deposit of Bengalun River, East Kalimantan Herman Darman
Berita Sedimentologi Vol 10, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1790.987 KB) | DOI: 10.51835/bsed.1998.10.1.274

Abstract

The Bengalon River is located in East Kalimantan, close to the northeastern margin of the Kutei Basin. A thick Paleogene and Neogene sedimentary package occur in this area, ranging from deep marine to fluviomarine depositional environments. This short note discusses the Early Miocene deep marine carbonates, particularly the calci-turbidite deposits.
Book Review: Sequence Stratigraphy and Characterization of Carbonate Reservoir Herman Darman
Berita Sedimentologi Vol 10, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (585.81 KB) | DOI: 10.51835/bsed.1998.10.1.279

Abstract

Sequence Stratigraphy and Characterization of Carbonate ReservoirBy Charles Kerans and Scott W. Tinker (1977), 130 p., Published by SEPM (Society for Sedimentary Geology) Short Course Note No. 40l 1731 E. 71st Street, Tulsa, OK 74136-5108. Fax: (1-918)-493-2093; http:\\www.sepm.org; ISBN 1056576-040-9; Price US$34 (member), US$48 List

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