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• W2028446605 abstract "The geoid, an equipotential surface of Earth’s gravity field, reflects the distribution of mass within the planet and hence a variety of geodynamic processes. Because these data are dominated by sublithospheric processes, notably mantle convection, they have not played a major role in the ongoing debate concerning models of the thermal evolution of oceanic lithosphere. Application of spatial filtering to the age derivative of the geoid, however, extracts an age-dependent signal which reflects lithospheric thermal evolution. The data are much better fit by a thin (about 100 km thick) thermal plate than by a cooling halfspace, and so provide a valuable constraint complementary to and consistent with the variations in oceanic depth and heat flow with age." @default.
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• W2028446605 date "1999-12-01" @default.
• W2028446605 modified "2023-10-16" @default.
• W2028446605 title "Extraction of a lithospheric cooling signal from oceanwide geoid data" @default.
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• W2028446605 doi "https://doi.org/10.1016/s0012-821x(99)00247-2" @default.
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