Pemodelan Sesar Pasca Gempa Dengan Inversi Data Gravitasi Time Lapse

Authors

Muhammad Zuhdi , Muhammad Taufik , Sutrio Sutrio , Syahral Ayub

DOI:

10.29303/jpft.v5i1.1109

Published:

2019-06-25

Issue:

Vol. 5 No. 1 (2019): Januari - Juni

Keywords:

Modeling, Gravity, Inversion, Time-lapse

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How to Cite

Zuhdi, M., Taufik, M., Sutrio, S., & Ayub, S. (2019). Pemodelan Sesar Pasca Gempa Dengan Inversi Data Gravitasi Time Lapse. Jurnal Pendidikan Fisika Dan Teknologi, 5(1), 156–161. https://doi.org/10.29303/jpft.v5i1.1109

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Abstract

Time lapse or 4D gravity is the development of gravity methods with the fourth dimension is time. This method is characterized by repetitive measurements over a period of time using a high-precision gravity measuring device (gravimeter) which is supported by high accuracy measurement of position. In the case of a fault that triggers an earthquake, layers that have a different density between layers will have the effect of changing the measured value of the gravitational field on the surface. The difference in the value of measured gravity before and after the occurrence of a fault as a result of an earthquake is what gives the value of time lapse gravity. The model of position displacement of the layers before and after the earthquake, provides a model of density between times whose gravitational anomalies can be calculated by forward response. The response of time-lapse forward model (synthetic data) is then optimized to obtain an inversion model. Inversion programming is made using the Mathlab program which is based on the semi-infinite horizontal slab equation. The model parameters that are optimized are horizontal position, depth, and amplitude factor of faulted layers. The program testing on 3 different synthetic data shows that the fastest optimization was obtained in the 7th iteration step. The smallest RMS error from the 3 models was 1.23. 10-5. This inversion program can be applied to time lapse gravity anomalies results of measurements in the field in active fault zones before and after the occurrence of an earthquake

References

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Dafis, K., Li, Y., and Batzle, M., 2008, ââ¬Â Time-lapse gravity monitoring: A systematic 4D approach with application to aquifer storage and recoveryââ¬Â GEOPHYSICS,VOL. 73, NO. 6 _NOV-DEC 2008_; P.WA61ââ¬âWA69, 13 FIGS. 10.1190/1.2987376

Zuhdi, M., Sismanto, Setiawan, A., Setyowiyoto, J., Susilo, A., Sarkowi, M. Radial Derivative and Radial Inversion for Interpreting 4D Gravity Anomaly Due to Fluids Injection Around Reservoir,TELKOMNIKA, Vol.16, No.6, December 2018, pp.2855~2863.

Kadir, W. G. A., 1999, ââ¬ÅSurvey Gravitasi 4D dan dinamika Sumber Bawah Permukaanââ¬Â: Proceeding Himpunan Ahli Geofisika Indonesia, 94-99.

Grandis. H.. Pengantar pemodelan Inversi Geofisika. Institute Teknologi Bandung, Himpunan Ahli Geofisika Indonesia, Bandung, p105-113,2009

Author Biographies

Muhammad Zuhdi, FKIP Universitas Mataram

I was born in Yogyakarta at December 29th, 1970. Graduated from Geophysics Dept. FMIPA UGM Yogyakarta in 1998. Master degree at Geophysics Dept, FIKTM ITB Bandung. I now teach physics in Universitas Mataram.

Muhammad Taufik, Program Studi Fisika, Universitas Mataram

Sutrio Sutrio, Program Studi Fisika, Universitas Mataram

Syahral Ayub, Program Studi Fisika, Universitas Mataram

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