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 8 Documents
Search results for , issue "Vol 12, No 1 (1999)" : 8 Documents clear
Sedimentary Facies of the Mahakam Delta: Comparison between the Modern and the Miocene A. Wiweko; B. Giriansyah
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2382.887 KB) | DOI: 10.51835/bsed.1999.12.1.265

Abstract

The Mahakam Delta is located on the eastern coast of Kalimantan Island, some 50 km south of the equator. The coastline of this area is oriented NNE-SSW, and is open to the Makassar Straits which are about 200 km wide, separating Kalimantan and Sulawesi.Field studies in the modern Mahakam Delta have been conducted by several workers. G.P. Allen, in 1974, conducted fieldwork to acquire a preliminary understanding of the sedimentary framework and characteistic facies distribution. The work was based on field observation, sediment sampling by using a Berthois hand dredge (surface sediment sampling) and coring devices (up to 2-4 meters depth), and water samples. In 1975, a second phase of study was conducted involving a coring program on the modern Mahakam Delta. The objective was to study the major geometrical characteristics and facies patterns of the formations. Additional coring program was conducted in 1976, which consisted of a number of shallower auger holes of up to 10 metres depth, and surface sediment samples. Allen (1992) conducted fieldwork in the large mouth bar system adjacent to Muara Bujit. The study was based on surface sediment sampling and shallow coring (up to 6 metres depth) to determine the geometry, facies patterns and internal architecture of a distributary mouth bar. The second phase of this work was done in 1993 and focused on the crest of the active distributary mouth bar to determine the detailed facies pattern, reservoir architecture and heterogeneity within the bar. The lengths of the vibracores used in this work were insufficient to determine in detail the thickness and geometry of the bar system. Therefore, coring campaign was again conducted in 1997, with drilling platform capable of drilling to depths of 20 m.Results of several studies conducted in the modern Mahakam sediments were then compared with facies analysis of the Miocene cores to understand any differences in terms of depositional energy between the modern and the Miocene sediments.
George P. Allen Bibliography Berita Sedimentologi
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1243.885 KB) | DOI: 10.51835/bsed.1999.12.1.271

Abstract

-
Comparison of Paleo-Mahakam Delta with Other Delta Systems F. Hasan Sidi
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2509.372 KB) | DOI: 10.51835/bsed.1999.12.1.266

Abstract

The Middle to Upper Miocene delta system in Kutai Basin is compared with several published delta models in this article. The modern day Mississippi has been taken to represent fluvial-dominated deltas, Colorado delta in the Gulf of California for tide-dominated delta, and the Rhone delta for the wave-influenced comparison.
Book Review: Sedimentation in the Modern and Miocene Mahakam Delta Dyah Tribuanawati
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (560.314 KB) | DOI: 10.51835/bsed.1999.12.1.272

Abstract

Sedimentation in the Modern and Miocene Mahakam DeltaBy: George P. Allen and John L. Chambers (1998), 236 p., Published by IPA (Indonesian Petroleum Association).
Salinity of the Modern Mahakam Delta, East Kalimantan Ateng Surachmat
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1784.301 KB) | DOI: 10.51835/bsed.1999.12.1.267

Abstract

As one of the most prolific basins in Indonesia, Kutai Basin has been well explored. A lot of research has been run and millions of dollars has been spent in order to have a better understanding the basin setting. One of the key aspects to understand the Kutai basin is to fully understand the modern Mahakam Delta, including its sedimentary source, depositional energy, reservoir behaviour and some other important aspects.The salinity study of modern Mahakam was performed as part of the regional study to understand the modern delta better. The Mahakam river waters were samples during the LSU (Louisiana State University) Mahakam Delta Study in 1994, whilst the project itself was funded by VICO Indonesia, UNOCAL and TOTAL Indonesie.
Deltaic Reservoir Partitions and Connectivity Herman Darman
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2403.663 KB) | DOI: 10.51835/bsed.1999.12.1.268

Abstract

A major part of the oil in the world produced from sandstone reservoirs has been from ancient delta systems. In general deltaic sands occur farther down dip than any other type of sand and they have relatively high recovery efficiency. Detail depositional environment study on deltaic reservoirs is important to create a model showing the distribution of reservoir properties that affect fluid flow. This article discussed the geometry and connectivity of deltaic reservoirs.
Bulungan Delta Clastic Wedges Winaldy Winaldy
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (581.961 KB) | DOI: 10.51835/bsed.1999.12.1.321

Abstract

Most of the gas and oil fields within the greater N.E Kalimantan basin are discovered in Tarakan subbasin. The Tarakan subbasin, the most productive subbasin, developed significantly during Middle Miocene to Pliocene when accommodation space for an increased volume of deltaic sediments was created due to a combination of basin subsidence and gravity induced listric faulting. However, the uplift of the western basin margin that had begun after Late Early Oligocene and continued into Miocene created shallower depositional conditions in the northern part of the basin (Tidung and Tarakan subbasins). The newly emergent area to the west formed constructive deltas that prograded from west to the east. Nevertheless, in the southern area (Berau and Muara subbasins) the depostion was under stable condition whereby platform carbonates and deeper marine sediments filled the region.
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

Abstract

-

Page 1 of 1 | Total Record : 8