Baasanbat
13/20 Azimuthal variations of the crustal structure for single station

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【ノート】
In this slide we can see azimuthal variation of the crustal structure beneath single station. N012 could have thicker transition zone between lower crust and mantle, others have narrow transient zone Low velocity zone in some azimuth. Azimithal variation due to heterogeneity. Crustal structures obtained from RFs from neighbor nodes have similar features (N011 N012) (N062 N063 N064) etc.