cover
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
Morpho-bathymetric features of the Southwest Celebes Sea Tiranda, Herwin
Berita Sedimentologi Vol 48, No 1 (2022)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2627.588 KB) | DOI: 10.51835/bsed.2022.48.1.389

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The Southwest Celebes Sea lies within the region of Celebes Sea (also known locally as Sulawesi Sea)-Makassar Strait gateway which is controlled by active tectonic of North Sulawesi Trench and Palu-Koro Fault zone. In addition, this region is the major inter-ocean route of Indonesian Throughflow (ITF). Using the high-resolution multibeam bathymetry data supplemented with 2D seismic profiles, this study describes major morpho-bathymetric features that can be observed within the Southwest Celebes Sea. There are 4 types of morpho-bathymetric features: structural features, erosional features, gravitational features, and depositional features. The dominant structural related tectonic features and gravitational features mainly occur in the North Sulawesi Fold-Thrust Belt associated with the formation of the North Sulawesi Trench and Palu-Koro Fault zone. Whereas, to the northern part, the deeper area of the Celebes Sea and the region on the west are mainly controlled by erosional and depositional features.  The identification of morpho-bathymetric features provides useful information for basin analysis study and present-day or future offshore activities such as infrastructure engineering related to geohazard potential caused.
Stratigraphic Analysis Base on Logs and Cores: An Overview Rovicky Dwi Putrohari
Berita Sedimentologi Vol 13, No 1 (2000)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (5326.606 KB) | DOI: 10.51835/bsed.2000.13.1.260

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Volcano Tourism of Mt. Rinjani in West Nusa Tenggara Province, Indonesia: a Volcanological and Ecotourism Perspective Rachmat, Heryadi
Berita Sedimentologi Vol 25, No 1 (2012)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (744.963 KB) | DOI: 10.51835/bsed.2012.25.1.177

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Indonesia has nearly 500 volcanoes and 129 of them are currently active. The active volcanoes are spread out along a 7000 km volcanic belt from Sumatra to Java, Bali, Nusa Tenggara, Banda, Halmahera and Sulawesi. Each volcano possesses its own natural characteristics that usually include beautiful landscapes and sceneries, fresh air and fertile lands. One of the volcanoes is Mount (Mt.) Rinjani (+3726 m) in Lombok island, West Nusa Tenggara. It is the second highest volcano in Indonesia after Mt. Kerinci (+3800 m) in Sumatra. Mt. Rinjani is situated at latitude 8°25' S and longitude 116°28' E. The Rinjani volcano complex has potential to be developed for volcano tourism and natural volcanic museum.Currently, vulcano tourism in Indonesia is still poorly developed and it relies on resources-based tourism only, not on knowledge-based tourism. Now is the moment for volcano tourism stakeholders, including travel guides, to prepare themselves by gaining more knowledge, specifically in term of scientific knowledge of a volcano and its environment. By doing so, they can make volcano more interesting as a tourist attraction and more appealing to both domestic and foreign tourists. The tourists eventually can have better understanding of a volcano including the landscapes, sceneries and panoramas, calderas, lakes, hotsprings, waterfalls, caves, etc.This paper discusses the volcano-tourism potential of Mt. Rinjani, focusing on volcanic and geological aspects as the main tourist attraction, and environmental aspect as a secondary attraction. The volcano-tourism attractions can include specific or general activities, depending on a visitor's interest, for examples for recreation, adventure or cultural activities.
Seismic Expression of Paleogene Talangakar Formation - Asri & Sunda Basins, Java Sea, Indonesia Dwandari Ralanarko; Deni Wahyuadi; Pranowo Nugroho; Wrahaspati Rulandoko; Ildrem Syafri; Abdurrokhim Almabrury; Andi Agus Nur
Berita Sedimentologi Vol 46, No 1 (2020)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (4935.021 KB) | DOI: 10.51835/bsed.2020.46.1.58

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The Asri and Sunda Basin are located offshore Southeast Sumatra under the SE Sumatera Production Sharing Contract (PSC). Currently, Pertamina Hulu Energi OSES operates in the Asri and Sunda Basins, known as Southeast Sumatra (SES) Block. As one of Indonesian prime oil and gas producing area in the past 50 years, these basins have produced cumulatively more than 1,500 MMBOE with an average of 90,000 BOPD. Both Asri and Sunda Basins are part of a series of Cenozoic half grabens developed on the Asian continental margin, that have occupied a retro arc setting since early Neogene times.Hydrocarbon exploration activities in the offshore southeastern Sumatra began with a signed agreement of Contract Sharing between IIAPCO (Independent Indonesian American Petroleum Company) and Pertamina on 6 September 1968.The contract area included the offshore areas east of Sumatra and south of Bangka - Belitung Islands, covering an area of 124,000 km2. After the final relinquishment in 2008, the current PSC boundary covers an area of 5,851 km2.This paper presents the results of integrated petroleum geosciences framework, its implications for Oligo-Miocene reservoirs and hydrocarbon prospectivity of the basins using near field exploration approaches. A four-fold division comprising rift initiation, rift climax, immediate post rift and late-post rift stages of basin evolution characterize the basin filling. Seismic expression of these kinematic units gives an idea about the linkage of their deposition with different stages of rift evolution. The present study has also identified a new potential play concept in Oligo -Miocene reservoirs.
Recent Agglutinated Foraminiferal Trends and Assemblages of the Sedili Besar River and Its Adjacent Offshore Area, Southeastern Peninsular Malaysia Mahani Mohamed; Sanatul Salwa Hasan; Shamsudin Jirin
Berita Sedimentologi Vol 29, No 1 (2014)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2076.539 KB) | DOI: 10.51835/bsed.2014.29.1.144

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The Sedili Besar River is strongly tidally influenced and its lower areas reach into a well-developed estuary. It enters the South China Sea along the wave-dominated southeastern coast of the Malay Peninsula. A total of 103 surface sediment and 48 shallow core samples from the tidal part of the river and the adjacent offshore area of Jason Bay were studied for Recent foraminiferal assemblages. The distribution of the agglutinated foraminifera shows abundance trends from the river estuary to the shallow marine offshore. Calcareous forms increase with water depth, but agglutinated foraminifera show a reverse trend.Five biofacies zones can be differentiated based on the abundance and species diversity of the dominant agglutinated foraminifera. These coincide with the upper brackish intertidal, lower brackish intertidal, estuary mouth, beach/nearshore and inner shelf depositional settings. Identification of the assemblages within the rock record from the Malay Basin and elsewhere will help considerably in a more precise characterization of the paleoenvironments of hydrocarbon reservoir intervals.
Cultural and geological heritage in time elapsed during historical Kingdoms in Yogyakarta Special Region, Indonesia Mulyaningsih, Sri
Berita Sedimentologi Vol 47, No 3 (2021)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (981.246 KB) | DOI: 10.51835/bsed.2021.47.3.359

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Yogyakarta, Indonesia is known for its kingdom government system for all its living history; since 8-10th century Mataram Hindu-Buddhist temples to the present Muslim Ngayogyokarto Hadiningrat. Those stretch of history resulted in many artefacts and chronicles. A cultural imaginary line that linking Merapi Volcano in the north and the Indian Ocean in the south through the Yogyakarta Palace in the middle has a sacral geo-cultural heritage, explaining a prosperity gentle volcanic town, a beautiful scheme of the open panoramic features with several temples standing on the plain and mountainous landscapes in between the rest of earthquakes and the volcanic eruptions. Many temples were partly buried under volcanic materials, and some others show evidence of being shaken several times by earthquakes. Boulders of volcanic materials varying in size and shapes are present in the plain of Yogyakarta, near Cangkiringan, Ngemplak and Ngaglik. Landslides exposed many geological features, such as faults, rock formation and stratigraphy, and some unstable slopes. Cultural and geological heritages at Yogyakarta Region were created over the time.
Geological Features Observations in Eastern Indonesia Based on Selected P3GL Seismic Data: A Report from FOSI-P3GL Seminar, Cirebon, January 31, 2018 Herman Darman; Ricky Andrian Tampubolon; Mellinda Arisandy
Berita Sedimentologi Vol 40, No 1 (2018)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3410.437 KB) | DOI: 10.51835/bsed.2018.40.1.82

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On January 31st, 2018, FOSI (Indonesian Sedimentologists Forum) organized a one day seminar in Cirebon (West Java), hosted by the Marine Geological Institute of Indonesia (or P3GL: Pusat Penelitian dan Pengembangan Geologi Kelautan). P3GL is a government institution which operates research vessels called Geomarin III. Their surveys typically include seismic acquisition, magnetic data acquisition and seafloor sediment sampling in Indonesian water. The seminar was aimed to provide an overview of their data to the geoscience community, especially those in the petroleum industry as the data may help petroleum exploration activities in Eastern Indonesia. This article focuses on selected seismic data which were presented during the seminar.
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

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Short Note: Mineral Composition of Eocene and Miocene Sandstones in Java Island Herman Darman; Budi Muljana; J. T. van Gorsel
Berita Sedimentologi Vol 26, No 1 (2013)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1404.733 KB) | DOI: 10.51835/bsed.2013.26.1.167

Abstract

A number of studies discuss the mineral compositions of Cenozoic sandstones in Java Island, Some sandstones are dominated by quartz, derived from granitic and/or metamorphic basement terrains or reworked sediments; many others are dominated by lithics and plagioclase feldspars derived from andesitic volcanics. The distribution of these two end-members varies through space and time, and has not been systematically been document for all of Java.The purpose of this short note is to contribute to the subject of Java sandstone provenance by summarizing quantitative analyses on sandstone compositions in the recent studies by Muljana and Watanabe (2012), Darman (1991), Siemers et al (1992) and Smyth et al (2008) and provide some additional data points as QFL (Quartz- Feldspar- Lithics) ternary plots.
IPA Field Trip ke Bengkulu Basin Berita Sedimentologi
Berita Sedimentologi Vol 5, No 1 (1997)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (998.159 KB) | DOI: 10.51835/bsed.1997.5.1.304

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Field trip yang diselenggarakan dalam rangka IPA Convention 1996, diselenggarakan di Bengkulu. Field trip yang disertai oleh 30 orang ini dipimpin oleh Bpk Berlian dan Sudarman dari Lemigas. Meskipun field trip ini dilaksanakan hampir satu tahun yang lalu, namun sayang rasanya jika hanya dinikmati oleh sedikit orang saja. Oleh karena itu kami tulis di sini agar lebih banyak orang yang dapat menikmatinya.