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- W1979821812 abstract "The dynamic shear modulus of unconsolidated marine sediments is small but nonzero. Shear waves will propagate in the sediments, but only at very slow speeds. The compressional wave speed is increased as much as 5% by the nonzero modulus. As a suspension of clay particles settles and collects into a gel-like material, the dynamic shear modulus increases. This initial development of sediment frame structure has been observed by measuring shear wave speed. Several stages in the development process can be described from these results." @default.
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- W1979821812 date "1976-11-01" @default.
- W1979821812 modified "2023-09-23" @default.
- W1979821812 title "Shear waves in unconsolidated sediments" @default.
- W1979821812 doi "https://doi.org/10.1121/1.2003422" @default.
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