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DEPARTMENT OF GEOLOGY RICE UNIVERSITY, HOUSTON, TEXAS
Abstract
Leaking modes are little influenced by the presence of a low
layer. The lattice-like structure of the phase-velocity curves occurs for a two-layer model as well as for a six-layer one. The excitation tends to be high where phase-velocity curves cross (or approach) each other. Both normally and inversely dispersed wave trains are predicted; the agreement with the observations varies from fair to good.
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