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- W2052096578 abstract "A uniformly valid mathematical formalism is developed to study the secular motions of the rotational axis of a layered viscoelastic earth due to seismic excitation. The changes required for implementing the formulation within the framework of the faulting problem. The rationale of adopting the chosen nrheological model, which contains a low-viscosity zone beneath the lithosphere and is based on linear Maxell constitutive relationship, is discussed. The impact of this low-viscosity channel on thhe two families of relaxation time, governing both isostatic readjustment and rotational processes, is considered. It is found that the polar motions depend sensitively on the viscosity structure of the asthenosphere and not at all on the underlying mantle. A gloal low-velocity zone with short-term asthenospheric viscosities less than about 5 x 10 to the 18th Pa-s and widths greater than 50 km is ruled out." @default.
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- W2052096578 date "1985-01-01" @default.
- W2052096578 modified "2023-10-18" @default.
- W2052096578 title "Transient polar motions and the nature of the asthenosphere for short time scales" @default.
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- W2052096578 doi "https://doi.org/10.1029/jb090ib05p03559" @default.
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