Baasanbat 18/20 Low velocity layer in upper crust

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Resulting velocity models for station U06M 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. There are similar velocity models from neighbor nodes. (N011 N012) (N062 N063 N064) etc.

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Baasanbat

18/20 Low velocity layer in upper crust