Fig. 1From: Effects of shallow-layer reverberation on measurement of teleseismic P-wave travel times for ocean bottom seismograph data Black Waveforms incident to the Moho. Red waveforms synthesized by convolving the crustal response for a crustal structure as shown in Table 1 with the incident waveform. Bandpass filter is applied at a central period of (a) 2.7 s, (b) 5.3 s, (c) 7.5 s, (d) 10.6 s, and (e) 21.2 sBack to article page