Broadband Seismic Deployments for Imaging the Upper Mantle Structure in the Lützow-Holm Bay Region, East Antarctica
Figure 6
(a) Back azimuth distribution for the depth converted receiver functions in the upper mantle compiled for all the GARNET stations. The number of receiver functions for each 15 azimuth range is shown in (b). The back azimuths are represented from Syowa Station (SYO) against the depth conversion points calculated for all the hypocenter-station pairs.
