Broadband Seismic Deployments for Imaging the Upper Mantle Structure in the Lützow-Holm Bay Region, East Antarctica

Figure 5

(left) Distribution of hypocenters of teleseismic events used for long-period receiver function analysis (solid circles) and SYO stations (solid triangles). (right) Distribution of P-S conversion depth points for 410 km (upper, crosses) and 660 km discontinuity (lower, open circles), respectively. Location of the conversion depth points was obtained by combining GARNET station positions in LHB and hypocenters of the utilized teleseismic events. Topographic depth variations of the upper mantle discontinuities are presented by the color contours (modified after Kanao et al. 2007 [1]).