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Abstract

A technique of layer velocity estimation tbrough semblance analysis was reported in Hadleyet al. (1988) and Landa et al. (1989). lts basic premise is that a coherency measure on unstacked seismograms reaches a maximum along reflection time trajectories that correspond to the correctly estimated velocity-depth model.

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/content/papers/10.3997/2214-4609.201407565
1994-07-24
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407565
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