# Spatio-Temporal Distribution of Ground Deformation Due to 2018 Lombok Earthquake Series
## 4 Discussion
\begin{table}
\begin{tabular}{l c c c c c c c c c} \hline \hline
**Location** & \begin{tabular}{c} **Number** \\ **of Pixels** \\ \end{tabular} & **Min** & **Max** & **Range** & **Mean** & **Median** & **Mode** & \
\begin{tabular}{c} **Least** \\ **Fre-** \\ **quent** \\ \end{tabular} & **Variance** &
\begin{tabular}{c} **Standard** \\ **Deviation** \\ \end{tabular} \\ \hline _29 July 2018_ & & & & & & & & & & \\ Mataram & 167,162 & \(-\)0.020 & 0.058 & 0.077 & 0.015 & 0.016 & 0.011 & \(-\)0.020 & 0.00034 & 0.006 \\ Pamenang & 46,767 & \(-\)0.148 & \(-\)0.026 & 0.122 & \(-\)0.083 & \(-\)0.084 & \(-\)0.117 & \(-\)0.148 & 0.000210 & 0.014 \\ Tampes & 86,079 & \(-\)0.109 & 0.055 & 0.165 & \(-\)0.032 & \(-\)0.040 & \(-\)0.063 & \(-\)0.109 & 0.000513 & 0.023 \\ Sukadana & 186,318 & \(-\)0.080 & 0.102 & 0.181 & \(-\)0.001 & \(-\)0.003 & \(-\)0.055 & \(-\)0.080 & 0.001096 & 0.033 \\ Sembalun & 140,887 & \(-\)0.163 & \(-\)0.021 & 0.142 & \(-\)0.095 & \(-\)0.095 & \(-\)0.104 & \(-\)0.163 & 0.000224 & 0.015 \\ Belanting & 120,364 & \(-\)0.103 & 0.031 & 0.134 & \(-\)0.033 & \(-\)0.032 & \(-\)0.035 & \(-\)0.103 & 0.000277 & 0.017 \\ \hline _5 August 2018_ & & & & & & & & & \\ Mataram & 176,680 & \(-\)0.073 & \(-\)0.002 & 0.071 & \(-\)0.040 & \(-\)0.040 & \(-\)0.053 & \(-\)0.073 & 0.000075 & 0.009 \\ Pamenang & 49,243 & 0.197 & 0.626 & 0.429 & 0.387 & 0.379 & 0.264 & 0.197 & 0.006355 & 0.080 \\ Tampes & 94,795 & 0.295 & 0.713 & 0.419 & 0.530 & 0.542 & 0.561 & 0.295 & 0.004501 & 0.067 \\ Sukadana & 202,391 & 0.224 & 0.507 & 0.283 & 0.374 & 0.382 & 0.277 & 0.224 & 0.003618 & 0.060 \\ Sembalun & 189,978 & 0.086 & 0.277 & 0.191 & 0.191 & 0.190 & 0.182 & 0.086 & 0.000202 & 0.014 \\ Belanting & 157,874 & 0.024 & 0.247 & 0.223 & 0.124 & 0.119 & 0.128 & 0.024 & 0.001304 & 0.036 \\ \hline _9 August 2018_ & & & & & & & & & \\ Mataram & 175,986 & \(-\)0.101 & \(-\)0.026 & 0.075 & \(-\)0.053 & \(-\)0.053 & \(-\)0.051 & \(-\)0.101 & 0.000009 & 0.003 \\ Pamenang & 70,863 & \(-\)0.338 & \(-\)0.150 & 0.188 & \(-\)0.225 & \(-\)0.220 & \(-\)0.224 & \(-\)0.338 & 0.000875 & 0.030 \\ Tampes & 159,333 & \(-\)0.161 & \(-\)0.067 & 0.094 & \(-\)0.121 & \(-\)0.121 & \(-\)0.127 & \(-\)0.161 & 0.000070 & 0.008 \\ Sukadana & 239294 & \(-\)0.148 & \(-\)0.055 & 0.094 & \(-\)0.105 & \(-\)0.106 & \(-\)0.114 & \(-\)0.148 & 0.000071 & 0.008 \\ Sembalun & 239,592 & \(-\)0.151 & \(-\)0.017 & 0.134 & \(-\)0.090 & \(-\)0.092 & \(-\)0.099 & \(-\)0.151 & 0.000115 & 0.011 \\ Belanting & 193,507 & \(-\)0.194 & \(-\)0.047 & 0.146 & \(-\)0.110 & \(-\)0.109 & \(-\)0.113 & \(-\)0.194 & 0.000146 & 0.012 \\ \hline _19 August 2018_ & & & & & & & & & \\ Mataram & 181,138 & \(-\)0.005 & 0.065 & 0.070 & 0.025 & 0.024 & 0.019 & \(-\)0.005 & 0.000027 & 0.005 \\ Pamenang & 78,016 & 0.056 & 0.284 & 0.228 & 0.160 & 0.163 & 0.148 & 0.056 & 0.001189 & 0.034 \\ Tampes & 166,333 & \(-\)0.008 & 0.092 & 0.100 & 0.046 & 0.045 & 0.039 & \(-\)0.008 & 0.00065 & 0.008 \\ Sukadana & 242,346 & 0.027 & 0.147 & 0.120 & 0.089 & 0.089 & 0.091 & 0.027 & 0.000298 & 0.017 \\ Sembalun & 249,290 & \(-\)0.017 & 0.204 & 0.221 & 0.092 & 0.090 & 0.082 & \(-\)0.017 & 0.001296 & 0.036 \\ Belanting & 185,297 & 0.111 & 0.475 & 0.364 & 0.265 & 0.275 & 0.284 & 0.111 & 0.002939 & 0.054 \\ \hline \hline \end{tabular}
\end{table} 
Table 2: Zonal statistics of displacement due to earthquakes in selected areas (Mataram city, Pamenang, Tampes, Sukadana, Sembalun, and Belanting). while PuSGen uses radar images on 25 July 2018 (master) and on 31 July 2018 (slave). The aftershock earthquake of 6.2 Mw on 9 August 2018 has never been analyzed before. Sentinel 1 imagery has been extensively used in global scale to analyze ground deformation due to single earthquakes [22; 23; 24; 25; 26]. DinSAR analysis derived from Sentinel 1 imagery on the Lombok earthquake series in Indonesia adds new insights. This small volcanic island with ultraplinian deposits and an active tectonic setting that was hit by multiple earthquakes has resulted in different ground deformation impacts on the spatio-temporal scale.