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Q3316767 - MaRDI portal

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    1984
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    hydrodynamic equations for ocean
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    subject to inhomogeneous time-dependent boundary condition at ocean floor
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    solution for flat earth tsunami mode excitation
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    ocean floor boundary condition derived from static response of elastic half-space to point moment tensor
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    model tsunami generation by earthquakes
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    normal mode techniques
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    point moment tensor earthquake source
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