Figure 2
From: Evidence for frozen melts in the mid-lithosphere detected from active-source seismic data
Observed and synthetic waveforms for OBSs 2–5. DR1 (arrows) indicates wide-angle reflection phases from the oceanic MLDs. Pn indicates refraction phases from the uppermost mantle. Observed and synthetic waveforms were band-pass filtered (5–20 Hz). Vertical axes were reduced using a velocity of 8.5 km s−1. The 900 km offset range of records from OBSs 2–5 are shown in Supplementary Fig. S1. Observed and synthetic waveforms show reflections from the oceanic MLD at distance of (a,b) 140–190 km (Fig. 3a), (c,d) 395–440 km and 400–460 km, (e,f) 465–490 km, (g,h) 410–495 km, and (i,j) 660–695 km.
