地球の弾性と粘性
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概要
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Observations of relaxation time <I>t</I> of deviation from perfect isostacy as a function of wave length λ will give us viscosity distribution within the earth. Preliminary studies of this kind suggest a low viscosity layer at a depth which coincides with the low velocity layer inferred from surface wave studies.
- 社団法人 東京地学協会の論文