Fig. 2From: Upper mantle structure beneath the Society hotspot and surrounding region using broadband data from ocean floor and islandsSchematic diagram of the two-station method. A, B Seismic stations. E is the source location. B′ is the projected point of B on the AE great circle. Gray broken lines indicate the Rayleigh wave front. Using the two-station method, the phase velocity between A and B′ is measured under the condition that the wave front propagates as a plane waveBack to article page