Fig. 11From: Seismic signature detection during the 2018 Anak Krakatau flank collapse and tsunami using seismic amplitudes from regional-scale monitoringExamination of sub-events T1–T3 identified in Fig. 10b. a Averaged source-normalized amplitudes with epicentral distance from Anak Krakatau for T1–T3 windows. b Maps of the averaged source-normalized amplitudes at each station. c Filtered seismograms from the CMJI station and the theoretical arrival times of body wave phasesBack to article page