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- W2150295959 abstract "Abstract The dispersion of earthquake waves propagated along the Pacific-Antarctic Ridge indicates that the crust is 6-7 km thick beneath the Ridge and slightly thinner beneath the adjacent deep water.Strong Love waves are recorded at Hallett Station from earthquakes on the Pacific-Antarctic Ridge, whereas strong Rayleigh waves are recorded from those on the East Pacific Rise; this difference is attributed to the source rather than to the medium.The structure of the Pacific-Antarctic Ridge appears to be intermediate between those found by other workers for the East Pacific Rise and the Mid-Atlantic Ridge." @default.
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- W2150295959 date "1964-08-01" @default.
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- W2150295959 title "Thickness Of The Earth's Crust Beneath The Pacific-Antarctic Ridge" @default.
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- W2150295959 doi "https://doi.org/10.1080/00288306.1964.10422100" @default.
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