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- W2035520253 abstract "The surface layer is replaced by a layer in which the velocity changes linearly with the depth, i.e. by a transition layer. A plane irrotational wave of arbitrary shape travels vertically upward and hits this layer. The multiples produced by differential reflections in the layer and by reflections at the free boundary are computed. From the third order on, these multiples look exactly like empirical reflections. The sum of all multiples is the solution of the differential equations of the problem, and has some formal mathematical similarity to diffraction phenomena known from optics." @default.
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- W2035520253 date "1961-09-01" @default.
- W2035520253 modified "2023-09-25" @default.
- W2035520253 title "SEISMIC WAVES IN A MATHEMATICAL MODEL OF THE SURFACE LAYER*" @default.
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- W2035520253 doi "https://doi.org/10.1111/j.1365-2478.1961.tb01516.x" @default.
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