Civil Insight: A Technical Magazine Volume 3 | Page 55

Shrestha P. et al. Civil Insight (2019) 51-56 Fig. 4. Earthquake epicenter data around Nepal (declustered data) 3.2) Seismicity parameters The earthquake catalog was further divided into two parts for the study: the first part consisted of data from 1800 to 1963 AD, and the second part consisted of data from 1964 to 2017 AD (Thapa & Wang, 2013). Source zones will produce earthquakes of different sizes – earthquake events up to the maximum earthquake, with smaller earthquakes occurring more frequently than that of the larger size events. The magnitude of completeness was obtained. Using Eqn (8) and Eqn (9), the ߚ-value and the activity rate ߣ are determined. From the value ofߣ, the ƒ -value can be calculated using Gutenberg-Richter recurrence relationship Eqn (7), for a minimum magnitude value. The various seismicity parameters obtained for the sources are shown in Table 2. Table 2. Seismic parameters of all seismic zones Source Model 1 SM SZ1 SZ2 SZ3 SZ4 SZ5 SZ6 2 SZ7 SZ8 SZ9 SZ10 SZ11 SZ12 ࢼ 1.92 1.92 1.92 1.92 1.92 1.92 1.92 1.92 1.92 1.92 1.92 1.92 1.92 ࣅ 1.40 2.41 2.89 2.41 2.29 1.27 0.87 2.41 1.55 1.49 2.11 2.59 1.22 „ 0.83 0.83 0.83 0.83 0.83 0.83 0.83 0.83 0.83 0.83 0.83 0.83 0.83 ƒ 3.48 3.72 3.80 3.72 3.69 3.44 3.27 3.72 3.53 3.51 3.66 3.75 3.42   ƒš  8.1 5.2 6.3 7.0 5.1 5.9 7.8 5.5 6.8 8.1 5.6 6.0 5.7 4) Conclusions The dam site of Upper Seti Hydropower Project was selected and all the available data on past earthquake events from 1255 to 2018 AD around Nepal were collected from various sources. For consistency, the earthquakes including main events and aftershock events were converted into a moment magnitude. The aftershocks were then decluttered using MATLAB (MATLAB, 2015) and referring to Gardner and Knopoff (1974) window algorithm. A basic assumption of seismic hazard analysis is that the recurrence law obtained from past seismicity is appropriate for the prediction of future seismicity. Thus, using Gutenberg-Richter recurrence law (1944), the seismicity parameters, ƒ and „ , were obtained. From this research, for Upper 55