Fig. 8From: A review of the seismotectonics of the Makran Subduction Zone as a baseline for Tsunami Hazard AssessmentsA shot gathered on onshore Makran. The crustal phase Pg can be observed up to 130 km. Note the strong overcritical reflections (Px) from 80 to 140 km. Y-axis is reduced time (Vred = 6 km/s); processing included only band pass filtering (2–10 Hz) and trace balancingBack to article page