Fig. 7From: Observation of the long-period monotonic seismic waves of the November 11, 2018, Mayotte event by Iranian broadband seismic stationsSemblance values, back-azimuth in degrees, and apparent slowness in s/km for radial components (a) and transverse components (b) of MVLP. Data from nine array stations (red triangles in Fig. 1) were used. The pair of vertical gray lines in a indicates the solution with the maximum semblance value of 0.75%Back to article page