Studi Prospek Reservoar Hidrokarbon Berdasarkan Karakteristik Petrofisika di Lapangan ‘X’ Cekungan Sebuku

  • Harsano Jayadi Program Studi Teknik Geofisika, Fakultas MIPA, Universitas Tadulako
  • Syahdan Ali Imran Program Studi Teknik Geologi, Fakultas Teknik, Universitas Tadulako
  • Widi Atmoko PT. Patra Nusa Data, Taman Tekno BSD Tangerang, Banten
  • Irianto Uno Program Studi Teknik Geologi, Fakultas Teknik, Universitas Tadulako
  • Icha Untari Meidji Program Studi Fisika, Fakultas Matematika dan IPA, Universitas Negeri Gorontalo

Abstract

The research was conducted to determine the hydrocarbon reservoir zone in the LIM-1 well, which was analyzed using quantitative and qualitative methods to assess the reservoir type involving several log data, including gamma ray (GR), neutron (NPHI), and density (RHOB). The quantitative analysis stage is the determination of hydrocarbon content by the crossover of NPHI log data, and RHOB log data with six target zones. The quantitative analysis stage in this study uses Interactive Petrophysics (IP) software version 3.5 on well LIM-1, also with target zone 1 only. The results obtained from qualitative and quantitative analysis at well LIM-1 show that there are three types of reservoirs in the study area from several target zones according to depth, which are dominated by oil, water, and gas.

References

[1] M. R. Harun, L. A. Sandria, A. S. Ilhami, A. Sukmatiawan, dan M. Razi, “Sandstone Reservoir Distribution of Cibulakan Formation Using Seismic Inversion Method: Extended Elastic Impedance (EEI), in Cemara Field, North West Java Basin,” 2013.
[2] M. Abduh, H. Jayadi, W. Atmoko, dan I. U. Meidji, “Analisis Petrofisika Untuk Penentuan Zona Prospek Reservoir Hidrokarbon di Lapangan ‘X’ Cekungan Banggai,” vol. 5.
[3] H. Jayadi, “Identifikasi Persebaran Litologi Reservoar Batupasir Menggunakan Analisis Seismik Inversi Impedansi Elastik di Lapangan Najlaa Formasi Cibulakan Cekungan Jawa Barat Utara,” Jurnal Fisika (Fisika Sains dan Aplikasinya), vol. 1, no. 2503 5274, hlm. 99–106, 2016.
[4] M. F. H. Kusuma, P. Lepong, dan E. Arifullah, “Studi Karakteristik Reservoir Berdasarkan Data Petrofisika (Studi Kasus Lapangan ‘X’ Lemigas Cekungan Sumatera Selatan),” Geosains Kutai Basin, vol. 6, no. 1, Art. no. 1, Feb 2023, doi: 10.30872/geofisunmul.v6i1.1044.
[5] G. E. Archie, “Introduction to Petrophysics of Reservoir Rocks,” hlm. 19, 1950.
[6] M. I. Nurwidyanto, I. Noviyanti, dan S. Widodo, “Estimasi Hubungan Porositas dan Permeabilitas Pada Batupasir (Study Kasus Formasi Kerek, Ledok,Selorejo),” BERKALA FISIKA, vol. 8, no. 3, Art. no. 3, Jul 2005.
[7] I. U. Meidji, D. G. E. Setiawan, A. P. Sari, W. Atmoko, dan H. Jayadi, “Tingkat Karakteristik Batuan Induk Sebagai Sumber Kandungan Minyak dan Gas Bumi : Studi Kasus Cekungan Lariang-Karama-Sulawesi Barat,” vol. 1, no. 2, 2023.
[8] D. Tiab dan E. C. Donaldson, Petrophysics: Theory and Practice of Measuring Reservoir Rock and Fluid Transport Properties. Gulf Professional Publishing, 2015.
[9] T. Darling, Well Logging and Formation Evaluation. Elsevier, 2005.
[10] M. I. Maulana, W. Utama, dan A. Hilyah, “Analisis Petrofisika dan Penentuan Zona Potensi Hidrokarbon Lapangan ‘Kaprasida’ Formasi Baturaja Cekungan Sumatera Selatan,” Jurnal Teknik ITS, vol. 5, no. 2, Art. no. 2, Feb 2017, doi: 10.12962/j23373539.v5i2.18238.
[11] A. Harsono, Evaluasi Formasi dan Aplikasi Log, Schlumberger, Edisi-8. Jakarta, 1997.
[12] J. Chen dan T. A. Dickens, “Effects of uncertainty in rock-physics models on reservoir parameter estimation using seismic amplitude variation with angle and controlled-source electromagnetics data,” Geophysical Prospecting, hlm. 14, 2008.
[13] P. E. Potter, J. B. Maynard, dan W. A. Pryor, Sedimentology of Shale: Study Guide and Reference Source. Springer Science & Business Media, 2012.
[14] R. Hall, “Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations,” Journal of Asian Earth Sciences, vol. 20, hlm. 353–431, 2002.
[15] J. A. Katili, “Large transcurrent faults in Southeast Asia with special reference to Indonesia,” Geol Rundsch, vol. 59, no. 2, hlm. 581–600, Feb 1970, doi: 10.1007/BF01823809.
[16] S. J. Calvert dan R. Hall, “Cenozoic evolution of the Lariang and Karama regions, North Makassar Basin, western Sulawesi, Indonesia,” PG, vol. 13, no. 4, hlm. 353–368, Nov 2007, doi: 10.1144/1354-079306-757.
[17] A. H. Satyana, “Re-Evaluation of the Sedimentology and Evolution of the Kais Carbonate Platform, Salawati Basin, Eastern Indonesia: Exploration Significance,” Annual Convention Proceedings, Indonesian Petroleum Association, hlm. 1–22, 2003.
[18] E. Biantoro, B. P. Muritno, dan J. M. Mamuaya, “Inversion faults as the major structural control in the northern part of the Kutai Basin, East Kalimantan,” vol. 1, hlm. 45–68, 1992.
[19] T. O. Simanjuntak, “Neogene plate convergence in Eastern Sulawesi,” Jurnal Geologi dan Sumberdaya Mineral, no. 25, hlm. 2–15, 1993.
[20] H. A. Kahfi dan J. Setiawan, “Geologi dan Estimasi Perhitungan Cadangan Gas Lapisan ”X”, Formasi Berai di Lapangan HR, Cekungan Makasar Selatan Berdasarkan Data Log Sumur dan Seismik,” Jurnal Ilmiah Geologi Pangea, vol. 3, no. 1, hlm. 101–108, 2016.
[21] J. Kupecz, I. Sayers, P. Tognini, A. Hilman, C. Tanos, dan D. Ariyono, “New Insights into the Tectono-Stratigraphic Evolution of the South Makassar Basin,” Proceedings, Indonesian Petroleum Association, 2013.
Published
2024-03-12
How to Cite
JAYADI, Harsano et al. Studi Prospek Reservoar Hidrokarbon Berdasarkan Karakteristik Petrofisika di Lapangan ‘X’ Cekungan Sebuku. GEOSAINS KUTAI BASIN, [S.l.], v. 7, n. 1, p. 13-21, mar. 2024. ISSN 2615-5176. Available at: <https://jurnal.fmipa.unmul.ac.id/index.php/geofis/article/view/1275>. Date accessed: 29 apr. 2024. doi: https://doi.org/10.30872/geofisunmul.v7i1.1275.
Section
Articles

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