| Summary: | This study intends to evaluate the possible correlation between the correlation dimension (D<sub>C</sub>) and the seismic moment rate for different late Quaternary active fault data, shallow crustal earthquakes, and GPS on the island of Sumatra Probabilistic Seismic Hazard Analysis (PSHA). The seismicity smoothing was applied to estimate the D<sub>C</sub> of active faults (D<sub>F</sub>) and earthquake data (D<sub>E</sub>) and then to correlate that with the b-value, which will be used to identify seismic hazard functions (SHF) along with the Sumatra Fault Zone (SFZ). The seismicity based on GPS data was calculated by the seismic moment rate that is estimated based on pre-seismic horizontal surface displacement data. The correlation between D<sub>F</sub>, D<sub>E</sub>, and the b-value was analyzed, and a reasonable correlation between the two seismotectonic parameters, D<sub>F</sub>-b, and D<sub>E</sub>-b, respectively, could be found. The relatively high D<sub>C</sub> coincides with the high seismic moment rate model derived from the pre-seismic GPS data. Furthermore, the SHF curve of total probability of exceedance versus the mean of each observation point’s peak ground acceleration (PGA) shows that the relatively high correlation dimension coincides with the high SHF. The results of this study might be very beneficial for seismic mitigation in the future.
|
|---|