Fig. 13From: Analysis of rotation sensor data from the SINAPS@ Kefalonia (Greece) post-seismic experiment—link to surface geology and wavefield characteristicsComparison of Love-wave phase velocity estimated using rotation sensor data [cf. Eq. (1)] and inferred from shear-wave velocity profiles (based on geophysical measurements) on both Kefalonia soft-soil and rock sitesBack to article page