Fig. 8From: Observation of the long-period monotonic seismic waves of the November 11, 2018, Mayotte event by Iranian broadband seismic stationsEstimated back-azimuth (black arrow) at each station using both Rayleigh and Love waves of MVLP (see text). Red arrows show the direction to the epicenter of MVLP (Lemoine et al. 2020) from each stationBack to article page