Analisis Kecepatan Gelombang S (Vs) Menggunakan Inversi kurva Horizontal to Vertical Spectral Ratio di Zona Patahan Opak, Bantul, Yogyakarta
DOI:
https://doi.org/10.24114/jiaf.v8i2.35090Keywords:
Gempabumi, Mikrotremor, Metode HVSR, VsAbstract
Model kecepatan bawah permukaan berdasarkan kecepatan gelombang geser (Vs) telah dilakukan di wilayah sesar Opak Bantul memotong ke arah Timur. Model kecepatan diperoleh dengan metode inversi kurva Horizontal-to-Vertical Spectral Ratio (HVSR). Model Vs yang diperoleh di zona patahan Opak Bantul, Yogyakarta menunjukkan adanya struktur patahan dengan bidang miring mengarah ke Timur Model Vs30 menunjukkan bahwa daerah bagian Barat dan Timur patahan Opak berasosiasi dengan endapan sedimen lunak. Endapan sedimen lunak tersebut dapat menyebabkan kerusakan yang signifikan jika terjadi getaran akibat pergeseran patahan (gempa bumi). Pada daerah bagian Timur Sesar Opak terjadi peningkatan nilai Vs yang menunjukkan adanya lapisan keras dari Formasi Nglanggran.References
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