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• W2115930863 abstract "Recent results from the analysis of postglacial rebound data suggest that the viscosity of the Earth's mantle increases through the transition region. Models which fit both relative sea-level and free air gravity data have viscosities which increase from a value near 1022 poise in the upper mantle beneath the lithosphere to a value of about 1023 poise in the lower mantle. In this paper we analyse the effect of deglaciation upon the Earth's rotation and thereby show that the observed secular trend (polar wander) evident in the ILS—IPMS pole path, and measurements of the non-tidal acceleration of the length of day, are both consistent with the viscosity profile deduced from postglacial rebound. The two analyses are therefore mutually reinforcing." @default.
• W2115930863 created "2016-06-24" @default.
• W2115930863 creator A5075937421 @default.
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• W2115930863 date "1981-09-01" @default.
• W2115930863 modified "2023-09-25" @default.
• W2115930863 title "Pleistocene deglaciation and the Earth's rotation: implications for mantle viscosity" @default.
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• W2115930863 doi "https://doi.org/10.1111/j.1365-246x.1981.tb04890.x" @default.
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