Analisis Tingkat Kerawanan Seismik Provinsi di Pulau Sumatera Menggunakan Parameter Gutenberg-Richter

Authors

  • Lola Amanda Program Studi Fisika, Fakultas Sains dan Teknologi, Universitas Islam Negeri Sumatera Utara, Jalan William Iskandar Ps V, Deli Serdang, Sumatera Utara 20371, Indonesia
  • Lailatul Husna Lubis Program Studi Fisika, Fakultas Sains dan Teknologi, Universitas Islam Negeri Sumatera Utara, Jalan William Iskandar Ps V, Deli Serdang, Sumatera Utara 20371, Indonesia
  • Ratni Sirait Program Studi Fisika, Fakultas Sains dan Teknologi, Universitas Islam Negeri Sumatera Utara, Jalan William Iskandar Ps V, Deli Serdang, Sumatera Utara 20371, Indonesia

DOI:

https://doi.org/10.36312/panthera.v6i3.1304

Keywords:

A-Value, B-Value, Earthquake, Maximum Likelihood, Sumatera Island

Abstract

Sumatra Island has complex geological conditions as it is located in a collision zone between the northward-moving Indo-Australian Plate and the relatively stable Eurasian Plate. The interaction of these two plates forms two main tectonic structures: the subduction zone off the western coast of Sumatra and the Sumatra Fault Zone (SFZ). The latter exhibits varying seismic activity that has not yet been clearly mapped. This study aims to assess the level of seismic vulnerability across Sumatra Island by dividing the region into nine zones using the a-value and b-value parameters based on the Gutenberg-Richter relationship. Earthquake data from the USGS and IRIS catalogs for the period 1924-2024 were processed through a declustering procedure and subsequently analyzed using the Maximum Likelihood method with the assistance of ZMAP v6 software. The results show that the a-value across Sumatra ranges from 2.1 to 5.1, while the b-value ranges from 0.545 to 0.868. North Sumatra records the highest a- and b-values, at 3.82 and 0.786, respectively. In contrast, West Sumatra shows the lowest values, with an a-value of 2.9 and a b-value of 0.623. These findings not only reveal variations in seismic activity across Sumatra Island, but also provide a more detailed zonation of seismic hazard based on the Gutenberg-Richter parameters, which can serve as a basis for disaster mitigation planning and the development of earthquake-resistant infrastructure.

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References

Alif, S. M., Cahyani, P. F., Anggara, O., & Rizqiansyah, A. (2022). Slip Rate of Kumering Fault in Lampung Province Calculated from GPS Data from 2007 to 2021. Jurnal Geosains dan Teknologi, 5(2), 83–90. https://doi.org/10.14710/jgt.5.2.2022.83-90

Chang, Y., Wang, R., Han, P., Wang, J., Miao, M., Zeng, Z., Wu, W., Jiang, C., Meng, L., Shi, H., & Hattori, K. (2025). b-Value Evaluation and Applications to Seismic Hazard Assessment. Entropy, 27(9), 1-19. https://doi.org/10.3390/e27090958

Dewi, E. A., & Prastowo, T. (2021). Studi Seismisitas melalui Penentuan Parameter a-Value dan b-Value di Wilayah Sumatera Barat. Inovasi Fisika Indonesia, 10(2), 48–58. https://doi.org/10.26740/ifi.v10n2.p48-58

Liu, X., Han, M., He, W., Li, X., & Chen, D. (2020). A New B Value Estimation Method in Rock Acoustic Emission Testing. Journal of Geophysical Research : Solid Earth, 125(12), 1-14. https://doi.org/10.1029/2020JB019658

Madlazim, & Lestari, N. I. D. (2022). Analisis Seismisitas dan Potensi Bahaya Bencana Seismik Pulau Sumatera Berdasarkan Data Gempa 1970–2020. Inovasi Fisika Indonesia, 11(2), 1–11. https://doi.org/10.26740/ifi.v11n02.p1-11

Pardo-Igúzquiza, E., & Dowd, P. A. (2024). Inference of the Gutenberg-Richter b-Value: New Insights and Results. Tectonophysics, 890(1), 1-18. https://doi.org/10.1016/j.tecto.2024.230486

Rasimeng, S., Helmi, M., Tugiyono, T., & Suharno, S. (2022). Fractal Dimension Analysis and Earthquake Repeated Period Estimation in the Southern Part of Sumatra Subduction Zone (Bengkulu-Lampung-Sunda Segment). Indonesian Journal on Geoscience, 9(3), 383–394. https://doi.org/10.17014/ijog.9.3.383-394

Risanti, H., Realita, A., Fahmi, M. N., Prastowo, T., & Madlazim. (2022). Seismicity Declustering Methods and Completeness Magnitude in Eastern Sunda Arc. Journal of Physics : Conference Series, 2377(1), 1-6. https://doi.org/10.1088/1742-6596/2377/1/012033

Scordilis, E. M. (2006). Empirical Global Relations Converting MS and Mb to Moment Magnitude. Journal of seismology, 10(1), 225-236. https://doi.org/10.1007/s10950-006-9012-4

Shearer, P. M. (2019). Introduction to Seismology (3rd ed.). Cambridge: Cambridge University Press.

Simanjuntak, V. C., Imran, I., Moestopo, M., & Setio, H. D. (2023). The Evolution of Seismic Design Provisions in Indonesia’s National Bridge Code. Journal of Engineering and Technological Sciences, 54(6), 1285-1304. https://doi.org/10.5614/j.eng.technol.sci.2022.54.6.14

Traitangwong, P., Khamsiri, S., & Pailoplee, S. (2024). Precursory Seismic Quiescence of Major Earthquakes Along the Sagaing Fault Zone, Central Myanmar. Geoscience Letters, 11(1), 1-12. https://doi.org/10.1186/s40562-024-00351-9

Woessner, J. (2005). Assessing Earthquake Catalogues and Magnitude of Completeness. Bulletin of the Seismological Society of America, 95(2), 684–698. https://doi.org/10.1785/0120040007

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Published

2026-07-03

How to Cite

Amanda, L., Lubis, L. H., & Sirait, R. (2026). Analisis Tingkat Kerawanan Seismik Provinsi di Pulau Sumatera Menggunakan Parameter Gutenberg-Richter. Panthera : Jurnal Ilmiah Pendidikan Sains Dan Terapan, 6(3), 1506–1515. https://doi.org/10.36312/panthera.v6i3.1304