Investigation of Sediment Layer Thickness Estimation at Bengkulu University Hospital Based on Microtremor Data

Authors

  • Andre Rahmat Al Ansory Program Studi Geofisika, Jurusan Fisika, Universitas Bengkulu
  • Hana Raihana University of Bengkulu
  • M Farid University of Bengkulu
  • Arif Ismul Hadi University of Bengkulu

DOI:

https://doi.org/10.20956/geocelebes.v8i1.28144

Keywords:

A0, f0, micotremor, sedimentary rocks, T0

Abstract

Bengkulu is the capital of Bengkulu Province and is located in the subduction zone between the Eurasian and Indo-Australian plates. Bengkulu is also close to the major faults of Sumatra, namely the Musi fault, the Ketahun fault, and the Manna fault. Therefore, regional planning and infrastructure development for earthquake mitigation is necessary. The purpose of this study is to estimate the thickness of the sedimentary layers in the construction zone of Bengkulu Hospital during the earthquake attenuation phase. This study is conducted by surface geological analysis using the HVSR method; data analysis using microtremor data. The microtremor data were analyzed using the HVSR method to obtain the amplification value (A0) and the dominant frequency (f0). HVSR analysis gave dominant frequency (f0) values from 5.1 to 5.8 Hz, amplification (A0) from 1.64 to 5.91 times, and dominant period (T0) from 1.49 to 2.81 seconds. The values of A0, f0, T0 are interpreted with reference to the literature and surface geology as a moderate risk of seismic vulnerability, characterized by moderate to weak sedimentation and moderate amplification values.

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Published

2024-04-01

How to Cite

Al Ansory, A. R., Raihana, H., Farid, M., & Hadi, A. I. (2024). Investigation of Sediment Layer Thickness Estimation at Bengkulu University Hospital Based on Microtremor Data. JURNAL GEOCELEBES, 8(1), 1 - 10. https://doi.org/10.20956/geocelebes.v8i1.28144

Issue

Vol. 8 No. 1: April 2024

Section

Articles

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