Fig. 3From: Effects of shallow-layer reverberation on measurement of teleseismic P-wave travel times for ocean bottom seismograph dataGlobal distribution of the time shift of teleseismic P-waves due to reverberations for crustal structures from CRUST2.0. Bandpass-filtered at a central period of a 2.7 s; b 3.8 s; c 5.3 s; d 7.5 s; e 10.6 s; f 15.0 s; g 21.2 s; h 30.0 sBack to article page