Fig. 4: End member synthetic test for mantle anomaly resolution and depth extent.
From: The Hindu Kush slab break-off as revealed by deep structure and crustal deformation
a, b Map view sections. c Profile along Fig. 2e. i Real data inversion results as in Figs. 2 and 3a for comparison. ii North-dipping slab scenario as in Fig. 3b. iii A model with similar geometry to (ii) but no mantle high-velocity zone exists between 100 and 180 km depth and deeper than 360 km depth. Local earthquakes, resolution limit and topography are plotted as in Fig. 2.
