Interpretasi Lingkungan Pengendapan Formasi Batuan Menggunakan Analisis Elektrofasies di Lokasi Tapak Puspiptek Serpong
Article Sidebar
Main Article Content
Abstract
The activity of subsurface material composing site foundation characterization is part of nuclear installation siting study. Characterization conducted by several methods, such as understanding the depositional environment of rock formations. As a segment of depositional environment interpretation method, facies model analysis based on electrofacies provides quicker information on depositional system of rock formation. Methodology applied is gamma ray log (log GR) interpretation using relative correlation between log shape variation and sedimentation facies. Based on the analysis, Bojongmanik Formation was deposited on marine-lagoonal environment with very low wave influence. Log GR that shows shape of funnel, serrated, and symmetry, indicate shoreface, lagoon, and tidal point bar facies. The direction of sedimentation, basin, and supply of Bojongmanik Formation interpreted relatively to the north. Serpong Formation deposited on meandering river system, and composed of point bar deposit, crevasse splay, and floodplain deposit. The result of analysis is expected to be guidance in further analysis related to the characterization of foundation materials.
Article Details
This work is licensed under a Creative Commons Attribution-ShareAlike 4.0 International License.
1. Introduction
By using or sharing content from EKSPLORIUM - Buletin Pusat Pengembangan Bahan Galian Nuklir ("the Journal"), you agree to follow these Terms and Conditions. The Journal's content is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike (CC BY-NC-SA) license. If you do not agree to these terms, please do not use the content.
2. How You Can Use the Content
-
Share: You can copy, share, and distribute the work, but only for non-commercial purposes.
-
Adapt: You can change, remix, or build on the work, as long as it is for non-commercial purposes and you share it under the same license (CC BY-NC-SA).
3. Attribution (Giving Credit)
When you use or share the content, you must:
-
Give proper credit to the author(s).
-
Mention the title of the work and the journal name.
-
Provide a link to the license (https://creativecommons.org/licenses/by-nc-sa/4.0/).
-
Indicate if you made any changes to the work.
4. Non-Commercial Use
You cannot use the work to make money or for any commercial activities. For example, you cannot sell or use the content in advertisements.
If you want to use the content for commercial purposes, you need to get permission from the author(s) or the publisher.
5. ShareAlike
If you make changes to the content (like creating a new version or remixing it), you must share your new version under the same CC BY-NC-SA license.
6. Exclusions
Some materials in the Journal may have different licenses or restrictions, such as third-party content (like images or datasets). You must respect the rules for those materials.
7. No Warranty
The content is provided "as is." The authors and publisher do not guarantee that the content is error-free or suitable for any specific purpose. Use the content at your own risk.
8. Modifications and Withdrawal of Content
The publisher and authors can update or remove content at any time. If content is removed, the previous versions will still follow these terms.
9. Ethical Use
You must use the content ethically and follow all relevant laws. This includes properly citing the original authors and not misusing the content.
10. Legal Compliance
You are responsible for making sure your use of the content follows the laws of your country. If you believe content violates your rights, please contact us.
11. Changes to Terms
These Terms and Conditions may be updated from time to time. Any changes will be posted on the Journal's website.
12. Contact Information
For questions about these Terms or for permission to use content commercially, please contact us at:
-
Email: eksplorium@brin.go.id
-
Website: https://ejournal.brin.go.id/eksplorium
Conclusion
By using the content from EKSPLORIUM - Buletin Pusat Pengembangan Bahan Galian Nuklir, you agree to follow these Terms and Conditions and the CC BY-NC-SA 4.0 International License.
References
Y. Cui, G. Wang, S. J. Jones, Z. Zhou, Y. Ran, and J. Lai, “Prediction of diagenetic facies using well logs e A case study from the upper Triassic Yanchang Formation, Ordos Basin, China,” Mar. Pet. Geol., vol. 81, pp. 50–65, 2017.
A. Nazeer, S. Ahmed, and S. Hussain, “Sedimentary facies interpretation of Gamma Ray (GR) log as basic well logs in Central and Lower Indus Basin of Pakistan,” Geod. Geodyn., vol. 7, no. 6, pp. 432–443, 2016.
L. Rolon, S. D. Mohaghegh, S. Ameri, R. Gaskari, and B. Mcdaniel, “Using artificial neural networks to generate synthetic well logs,” J. Nat. Gas Sci. Eng., vol. 1, pp. 118–133, 2009.
C. Betzler, T. Pawellek, M. Abdullah, and A. Kossler, “Facies and stratigraphic architecture of the Korallenoolith Formation in North Germany (Lauensteiner Pass, Ith Mountains),” Sediment. Geol., vol. 194, pp. 61–75, 2007.
International Atomic Energy Agency (IAEA), Geotechnical Aspects of Site Evaluation and Foundations for Nuclear Power Plants. Vienna, Austria, 2004.
J. He, W. Ding, J. Zhang, A. Li, and W. Zhao, “Logging identification and characteristic analysis of marine-continental transitional organic-rich shale in the Carboniferous-Permian strata, Bohai Bay Basin,” Mar. Pet. Geol., vol. 70, pp. 273–293, 2016.
M. Benvenuti and S. Del Conte, “Facies and sequence stratigraphic modeling of a Upper Pliocene – Lower Pleistocene fluvial succession (Valdelsa Basin, central Italy),” Sediment. Geol., vol. 294, pp. 303–314, 2013.
A. Roslin and J. S. Esterle, “Electrofacies analysis for coal lithotype profiling based on high-resolution wireline log data,” Comput. Geosci., vol. 91, pp. 1–10, 2016.
Ikatan Ahli Geologi Indonesia (IAGI), Sandi Stratigrafi Indonesia Edisi 1996. 1996.
R. G. Walker and N. P. James, Facies model: response to sea level change. Geological Association of Canada, 1992.
P. S. Momta and M. I. Odigi, “Reconstruction of the Depositional Setting of Tortonian Sediments in the Yowi Field, Shallow Offshore Niger Delta, Using Wireline Logs,” Am. J. Geosci., vol. 6, no. 1, pp. 24–35, 2016.
Q. K. Jadoon, E. M. Roberts, B. Henderson, T. G. Blenkinsop, R. A. J. Wüst, and C. Mtelela, “Lithological and facies analysis of the Roseneath and Murteree shales, Cooper Basin, Australia,” J. Nat. Gas Sci. Eng., vol. 37, pp. 138–168, 2017.
Abdurrokhim and M. Ito, “The role of slump scars in slope channel initiation: A case study from the Miocene Jatiluhur Formation in the Bogor Trough , West Java,” J. Asian Earth Sci., vol. 73, pp. 68–86, 2013.
B. Clements and R. Hall, “Cretaceous To Late Miocene Stratigraphic and Tectonic Evolution of West Java,” in Proceedings of Indonesian Petroleum Association, 2007.
S. Martodjojo, Evolusi Cekungan Bogor, Jawa Barat. ITB Bandung, 2003.
T. Turkandi, Sidarto, D. Agustiyanto, and M. Hadiwidjojo, “Peta Geologi Lembar Jakarta dan Kepulauan Seribu, Jawa.” Pusat Penelitian dan Pengembangan Geologi, Bandung, 1992.
S. H. Vaziri, F. T. Fürsich, and N. Kohansal-ghadimvand, “Facies analysis and depositional environments of the Upper Cretaceous Sadr unit in the Nakhlak area , Central Iran,” Rev. Mex. Ciencias Geol., vol. 29, no. 2, pp. 384–397, 2012.
M. Fachri, Djuhaeni, L. M. Hutasoit, and A. M. Ramdhan, “Stratigrafi dan Hidrostratigrafi Cekungan Airtanah Jakarta,” Bul. Geol., vol. 34, no. 3, pp. 169–190, 2002.
R. M. Delinom, A. Assegaf, H. Z. Abidin, M. Taniguchi, D. Suherman, R. Fajar, and E. Yulianto, “The contribution of human activities to subsurface environment degradation in Greater Jakarta Area, Indonesia,” Sci. Total Environ., vol. 407, no. 9, pp. 3129–3141, 2008.
Marjiyono, H. Suntoko, A. Soehaimi, Yuliastuti, and H. Syaeful, “Kelas Soil Daerah Sekitar Rencana Tapak Reaktor Daya Eksperimental (RDE) Serpong Dari Data Mikrotremor,” J. Pengemb. Energi Nukl., vol. 17, no. 1, pp. 57–66, 2015.
