Fig. 6From: Significant P wave conversions from upgoing S waves generated by very deep earthquakes around JapanR and T component seismograms of ground velocity for the 2010 Vladivostok event (Mw 6.8, 578 km depth) at a chain of F-net seismic stations along the Japanese islands, shown with solid symbols in Fig. 5. For each station, the epicentral distance is indicated in degrees, with the maximum amplitude in μm/s shown below in smaller type. The travel times of the major phases for the ak135 model are indicated on each trace. Traces are normalized by the maximum three-component energy in the time windowBack to article page