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Contact Name
Minarwan
Contact Email
minarwanx@gmail.com
Phone
+6281908602813
Journal Mail Official
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
Location
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 8 Documents
Search results for , issue "Vol 15, No 1 (2001)" : 8 Documents clear
Deep-water Gulf of Mexico Basin: An Overview of Its Petroleum Exploration F. Hasan Sidi
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (4209.039 KB) | DOI: 10.51835/bsed.2001.15.1.247

Abstract

The Gulf of Mexico Basin is one of the most prolific petroleum provinces in the world. The present-day deepwater portion of the Guld of Mexico has been explored since mid 1970's. Exploration and development activities have increased significantly during the last couples of years. Since then, over 600 wildcat wells have been drilled in the various deep-water plays in the basin, and industry has leased in excess of 4300 lease blocks covering a cumulative area of more than 38,700 square miles. This activity has been caused by several factors including significant discoveries in deep-water, outstanding reservoir performance in some these discoveries, innovative production techniques, and new Federal royalty relief.There have been 121 discoveries made in the province during the period from 1975 to the end of 1998 with the mean size of these discoveries is 96.5 MMBOE and the largest field found to date is Mars (720 MMBOE). Despite the abundance of drilling and leasing in the basin, some deepwater Gulf of Mexico plays are still in the unproven stage.
Turbidite Outcrops as Analogs for Deep-water Reservoirs: A Case from NW Borneo S. Back; J.J. Lambiase
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2733.345 KB) | DOI: 10.51835/bsed.2001.15.1.248

Abstract

Deep-water reservoirs around Borneo are currently an important target for hydrocarbon exploration. Data used to evaluate potential reservoir geometries and quality include quantitative reservoir from outcrop analogs.
Late Turbidite Paradigm: Dispute on Cinambo Outcrop as Turbidites? RMI Argakoesoemah
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (4234.738 KB) | DOI: 10.51835/bsed.2001.15.1.244

Abstract

Conoco Indonesia performed a one-day geological fieldtrip to Majalengka and Kadipaten, West Java in late November 2000. The trip was led by DR. Dardji Noeradi (ITB).Discussion below is a short observation of the outcrops seen in Cinambo with no intention to describe or interpret the details of the outcrops. It should be noted here that the short timing and condition during the fieldtrip was insufficient to further dig out geology of the area in more scientific manner. However, some critical points have been identified, two of them are, in fact, basic questions arose during and after the fieldtrip completed: (1) is there any turbidite sediments in Cinambo, and (2) how the sequences seen were deposited.To respond to there crucial questions above one need further investigation and deep observation. It may take at least three or four months in the field just to prepare at least a couple dozen, correlatable detailed measured sections, observe and collect sedimentary structures, with no model-driven at all in mind. Other months are to work in the laboratory to record lithology variations and changes through possibly of hundreds of thin sections of systemtic rock samples. This is not a rocket science. But why? Here it is.
Outcrops of West Crocker Formation - A Field Visit Mohammad Syaiful
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3299.141 KB) | DOI: 10.51835/bsed.2001.15.1.249

Abstract

West Crocker Formation is located in Northwest Sabah of Borneo (Kalimantan) Island. This formation was deposited during Late Palaeogene (Oligocene) and is undoubtedly the best exposed example of a classic submarine fan system in the Asian region.A field visit had been done in August 1999 to view the outcrops of West Crocker Formation. These have been well-exposed in Kota Kinabalu and its vicinity. In fact, the field trip had been held to also visit other Paleogene and younger Neogene rocks in Labuan Island and Brunei areas. In this text, only the outcrops of West Crocker Formation will be discussed.
Revisiting the Middle Baong Sand: Basin Floor Fan or Slope Fan in Origin? Siti Nur'aini; Soejono Martodjojo; Frank W. Musgrove; Jon Bon
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3828.721 KB) | DOI: 10.51835/bsed.2001.15.1.245

Abstract

The Baong Formation contains three lithology units, namely shale unit (lower part), sand unit (middle part) and another shale unit (upper parts). The middle part of Baong Formation is usually called as the Middle Baong Sand (MBS) because it was deposited between two deep-marine shale lithologies during the Middle Miocene time. The Middle Baong Sand is the first turbidite reservoir found in Indonesia. Two feeder systems of Baong Sand came from the Barisan Mountain and the Malaka Shelf.Several authors had interpreted the Middle Baong Sand in Duyung Well as basin floor fan sediments. The Baong Sand in North Lho Sukon Deep was concluded to be slope fan complex, whereas in Jambuaye Utara Well was interpreted to be highstand sediments. The interpretation of this unit was merely leaned on log signatures or seismic characters without considering their presence on the regional geologic setting. The aim of this study is to investigate the depositional model of the Baong Sand within the geological setting of North Sumatra Basin.
Book Review: Fine-Grained Turbidite Systems, AAPG Memoir 72 & SEPM Special Publication No 68 Berita Sedimentologi
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (279.179 KB) | DOI: 10.51835/bsed.2001.15.1.250

Abstract

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Turbidite Plays of Indonesia: An Overview Herman Darman
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3632.632 KB) | DOI: 10.51835/bsed.2001.15.1.246

Abstract

In the last decade significant advances in geologic understanding and exploration technology in Indonesia continue to reduce the risks associated with exploration and development in turbidite plays. New plays are defined based on recently acquired seismic and well data. Turbidite is becoming a very important play in Sumatra, Kalimantan, Java, and Irian.This paper will give a summary of the latest development on the geological concepts of the deep-water successions in Indonesia based on exploration data.
Report of 2000 FOSI Membership and Financial Progress Berita Sedimentologi
Berita Sedimentologi Vol 15, No 1 (2001)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (735.147 KB) | DOI: 10.51835/bsed.2001.15.1.251

Abstract

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