Fig. 4.From: A new algorithm for the detection of seismic quiescence: introduction of the RTM algorithm, a modified RTL algorithmTime variations of the RTL and RTM under the parameter sets #2 and #7 at the epicenter (136.69°E, 37.22°N) of the Noto Hanto Earthquake in 2007 in central Japan. Upper and lower panels represent the time variation of the RTL and RTM values. Thin and thick lines indicate #2 and #7, respectively.Back to article page