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Journal : Indonesian Journal on Geoscience

Sedimentation Process of Rambatan Formation in Larangan Brebes, North Serayu Range, Central Java Astuti, Bernadeta Subandini; Isnaniawardhani, Vijaya; Abdurrokhim, Abdurrokhim; Sudradjat, Adjat
Indonesian Journal on Geoscience Vol 6, No 2 (2019)
Publisher : Geological Agency

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17014/ijog.6.2.141-151

Abstract

DOI:10.17014/ijog.6.2.141-151Rambatan Formation in the western part of North Serayu Basin, Brebes, Central Java, comprises generally flysch facies of turbidite sediments deposited in a deep marine environment. This formation is equivalent to Merawu Formation found in the eastern part of the basin and deposited in the environment of tidal flat to subtidal. The turbidite sediments were highly controlled by a rapid downward movement taking place continuously during Early to Late Miocene. The variation of the depositional environment has been the object of this research which aims to understand the sedimentation process of Rambatan Formation in this type locality with a modern turbidite approach. Rambatan Formation was deposited in N13-N19, as a deep marine sediment channel, turbidite, and deep marine tidal zone. The sedimentation was affected by gravity flow and contourite. The sediments on N13-N14 were marked by turbidite sediments until Middle N17. The sediment supply increased on Middle N17, as a sediment filler on a channel marked by contourite mud layer (muddy slump) and debris flow, with sources from the north. The increase of sediment supply was followed by an environmental transformation from a deep marine channel into deep marine tidal area. In N19, the sediments were redeposited as turbidite sediment, starting with debris flow in Middle N18.
Characteristics of Arun Carbonate Reservoir and Its Implication To Optimize the Most Potential Gas Resource Zone In Arun Gas Field, Aceh, Indonesia Atmadibrata, Riza; Muslim, Dicky; Hirnawan, R. Febri; Abdurrokhim, Abdurrokhim
Indonesian Journal on Geoscience Vol 6, No 2 (2019)
Publisher : Geological Agency

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17014/ijog.6.2.209-222

Abstract

DOI:10.17014/ijog.6.2.209-222Since the discovery of major oil and gas reserves in carbonate rocks in the Middle East, carbonate reservoirs became important to the petroleum industry. Carbonate rocks have covered only 20% of the sedimentary rock records. However, carbonate reservoirs hold 50% of the world petroleum reserves. Arun Carbonate Reservoir is one of the biggest proven retrograde gas reservoirs in the world. After more than thirty years of production, Arun Carbonate Reservoir had an initial gas in place of 14.1 TCF residual hydrocarbon gas. The issue makes Arun Carbonate Reservoir became an interest to be studied for the development and production of hydrocarbon in other carbonate reservoirs in Indonesia. One of the fundamental topics to be studied is the characteristics of Arun Carbonate Reservoir itself. The characteristics of carbonate reservoir usually cause a lot of geologic and engineering problems in the development and production of hydrocarbon reserves. This paper aims to identify the characteristics of Arun Carbonate Reservoir and its implication to delineate the potential gas resource zone in the Arun Gas Field, Aceh, Indonesia. The data from sixteen wells have been examined through several multidiscipline studies: geophysics (well logging), geology (facies, lithology and diagenetic analyses), and petrophysics (core analysis). The result of this study shows that Arun Carbonate Reservoir (N5-N8) contains limestone 92%, 5% dolomite, and 3% dolomitic limestone (or other), and petrophysically have 16% porosity and 13.5 md permeability in average. Arun Carbonate Reservoir is divided into four facies (Reef, Near Reef, Inter Reef Lagoon, and Middle Shelf). Of four facies in Arun Carbonate Reservoir, only two facies which can be categorized as productive facies: Reef and Lagoonal Facies. The potential zones of hydrocarbon resources have vertically been documented in Arun Carbonate Reservoir.
Co-Authors Adhiperdhana, Billy Gumelar Adjat Sudradjat Adjat Sudradjat Adriano Mazzini Agus Nur, Andi Agustya Agustya Ajat Sudrajat Akbar, Muhammad Miftahul Andi Agus Nur Asep Mohamad Ishaq Shiddiq Atmadibrata, Riza Atmadibrata, Riza Bernadeta Subandini Astuti Bonar Tua Halomoan Marbun Brian Christiantoro Budi Muljana Budiana, Rahmat Christiantoro, Brian Dedi Kuswandi Dicky Muslim Dwandari Ralanarko Edy Sunardi Faisal Helmi Fatmayanti, Fera Febriwan Mohamad, Febriwan Febriwan Mohammad Febriwan Mohammad, Febriwan Fercanza, Frisdio Firman Herdiansyah, Firman Firstikara, Ghania Callysta Hardjowikarto, Dharliana Ayu Hastowo Resesiyanto Hendarmawan H Hendarmawan Hendarmawan Herlinawati H Hirnawan, R. Febri Hirnawan, R. Febri Ildrem Sjafri Ildrem Syafri Ildrem Syafri Ildrem Syafri Ildrem Syafri Irvan Sophian Ismawan Ismawan, Ismawan Iyan Haryanto Iyan Haryanto, Iyan Januar Arifin Johanes Hutabarat Karyono Karyono Lia Jurnaliah Marbun, Bonar Tua Halomoan Masturyono Masturyono Mohamad Solihin, Mohamad Morang, Febrika Situ Muhammad Kurniawan Alfadli mutiara mutiara Nisa Nurul Ilmi Nugroho, Dimas Andhi Nur Khairullah Nuraeni, Tia Nursasono, Danny Panji Ridwan Petra Wattimury Popi, Popi Prasetyo, Anggit Chandra R. Febri Hirnawan Rachma, Nabila Fathiyah Resesiyanto, Hastowo Reza Muhammad Ganjar Gani, Reza Muhammad Ganjar Ridho Kresna Wattimena Ridho Kresna Wattimena Riza Atmadibrata Rohimah, Sania Saida Ulfa Saputra, Akbar Wahyudi Adi Sari Widyastuti, Sari Savitri, Cindy Dhevayani Shiddiq, Asep Mohamad Ishaq Soffian Hadi Sudarsana, Muhammad Rizki Supriyanto Rohadi Syafi'i, Abdullah Vijaya Isnaniawardhani Wahyuningsih, Amelya Andini Wattimury, Petra Yoga Adriana Sendjaja, Yoga Adriana Yuyun Yuniardi Zahran, Raihan Zaki ZULFAHMI ZULFAHMI Zulfahmi Zulfahmi