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Unformatted text preview: V h V V V V h V x T + + = Applied Geophysics Refraction I Horizontal vs. vertical velocity contrasts A three-horizontal layer model can produce the same traveltime curve as a single horizontal layer over a vertical velocity contact 1/V 1 1/V 2 1/V 3 1/V 1 1/V 2a 1/V 2b Head wave continues into 2b...
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This note was uploaded on 01/07/2012 for the course PHYSICS 384 taught by Professor Wei during the Spring '09 term at SUNY Stony Brook.
- Spring '09