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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 282 Documents
Ulasan Singkat Buku: Sedimentation in Volcanic Settings Berita Sedimentologi
Berita Sedimentologi Vol 6, No 1 (1997)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (397.562 KB) | DOI: 10.51835/bsed.1997.6.1.298

Abstract

Sedimentation in Volcanic SettingsEditor: Richard V. Fisher and Gary A. SmithPenerbit/tahun: SEPM Special Publication No. 45, 1991Keterangan: 264 halaman, sampul kerasHarga: US$65 (SEPM Member); US$89 (List)
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
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

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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.
Short Note: Overview of the Baram Delta Province, Brunei Darussalam Arse K. Hay
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (535.362 KB) | DOI: 10.51835/bsed.1999.12.1.269

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Eocene Sediments in the South China Sea, precursor deposits of the Oligocene expansion? Franz L. Kessler; John Jong; Mazlan Madon
Berita Sedimentologi Vol 47, No 2 (2021)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2412.968 KB) | DOI: 10.51835/bsed.2021.47.2.319

Abstract

The stratigraphic record of Eocene in the Malaysian waters of the South China Sea is scarce; the few deep petroleum exploration wells and outcrops are located on the fringes of the SCS. Yet, despite the paucity of data we observe a variety of sediments that cover the range from fluviatile to (at least) neritic marine deposits. Whilst fluvial deposits dominate the Western Rim (Penyu, Malay basins), the Southern Rim (Sarawak) is characterized by deposits of a narrow and rapidly deepening shelf, with fluviatile, shallow marine clastics and carbonates passing seawards to outer shelf and neritic deposits. The proven record of the Eocene to-date is located in relatively small and deep sub-basins.  Possibly, the Eocene underlies additional areas of the SCS, but there is to-date no sufficient well data to offer further confirmation. The presence of Eocene strata on the margins of Sundaland is associated with an early phase of extensional and/or transpressional tectonism, probably acting as precursor movements related to the onset of rifting of the crust underlying the SCS.
Sedimentology of Coal Conglomerate Deposits within Channel Facies in Samarinda Region, East Kalimantan Herman Darman; Yahdi Zaim
Berita Sedimentologi Vol 17, No 1 (2002)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1604.159 KB) | DOI: 10.51835/bsed.2002.17.1.237

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The Power of Palaeocurrents: Reconstructing the Palaeogeography and Sediment Flux Patterns of the Miocene Sandakan Formation in Eastern Sabah Jon Noad
Berita Sedimentologi Vol 28, No 1 (2013)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2933.686 KB) | DOI: 10.51835/bsed.2013.28.1.153

Abstract

Up until now the use of palaeocurrents as a primary tool in establishing regional palaeogeography and sediment dispersal patterns in the ancient has been limited. An outcrop study on the Miocene Sandakan Formation in eastern Sabah identified five facies belts, subdivided on the basis of sedimentological and palaeontological data. More than 140 outcrop sections were measured over an area covering approximately 200 square kilometres. The facies were interpreted to have been deposited in settings ranging from ancient mangrove deposits through shoreface sediments and out into the open marine.More than 200 palaeocurrent readings taken on these facies allowed a clear picture to be built up of the sediment dispersion patterns across the palaeo-Sandakan Basin, passing from northward directed flow through mangrove channels into a longshore drift dominated shallow marine, coastal shelf. This gave way northwards to a storm dominated belt of tempestite deposits cut by rip current channels. Flow through these channels, driven by frequent storms, was northward directed. Further to the north more quiescent, open marine, muddy conditions prevailed. A sediment budget can be estimated using the sand fraction of the various lithofacies identified during the study.
Planktonic Foraminifera Biozonation of the Middle Eocene-Oligocene Kebo Formation, Kalinampu Area, Bayat, Klaten, Central Java Dian Novita; Didit Hadi Barianto; Moch. Indra Novian
Berita Sedimentologi Vol 31, No 1 (2014)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (7220.658 KB) | DOI: 10.51835/bsed.2014.31.1.125

Abstract

Research on foraminifera from the Paleogene volcanoclastics-dominated Kebo Butak Formation of Central Java is limited. A study was conducted in the Kalinampu and surrounding areas of Bayat, Klaten, Central Java. The study included measuring of three stratigraphic sections and geological mapping. The study area contains the Nampurejo pillow lava, which is considered to be the base of the Kebo-Butak Formation (part of the 'Old Andesites' complex of South Java), but its Middle Eocene age is older than previously assumed.Correlation and biozone interpretation allowed the recognition of 12 planktonic foraminifera zones, ranging in age from Middle Eocene (P11) to Early Miocene (N5). Depositional environments are all deep marine, ranging from lower bathyal to upper bathyal.
Ulasan Singkat Buku: Cycles and Events in Stratigraphy Berita Sedimentologi
Berita Sedimentologi Vol 7, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (381.968 KB) | DOI: 10.51835/bsed.1998.7.1.294

Abstract

Cycles and Events in StratigraphyEditor: G. Einsele, W. Ricken, A. SeilacherPenerbit/tahun: Springer-Verlag/1991Keterangan: 955 halaman, sampul kerasHarga: US$
A Simplistic Approach in Estimating Paleo- Bathymetry by Using Seismic Stratigraphic Features in Fluvial-Dominated Delta Agus Susianto
Berita Sedimentologi Vol 21, No 1 (2011)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (908.672 KB) | DOI: 10.51835/bsed.2011.21.1.209

Abstract

The advance of high resolution 3D seismic technology has enabled much detailed imaging not only for structural features, but also for detailed stratigraphic features. If we squeeze a little bit more out of seismic data, it can provide us some important information. Seismic stratigraphy analysis in a prograding delta setting can deliver simple yet useful tool in understanding the geological and depositional aspects from seismic data. Recognizing unique seismic stratigraphic pattern of each part of delta and their chronostratigraphic correlative unit will allow us to understand the depositional relief of ancient delta sequence observable in seismic. This article discusses how to do simple estimation of paleobathymetry in a fluvial dominated delta and its limitation. This is a little effort to make seismic interpretation more meaningful and much more fun.