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- W1986585184 abstract "The flexure of the lithosphere under a linear load such as at Hawaii, and before a trench such as in the Hokkaido rise—Kuril trench system are calculated assuming homogeneous visco-elasticity and (in the second case) a superimposed longitudinal compression. The well-established rigidity of plates on the million years scale implies a viscosity η ⩾ 1025 poises, and focal mechanisms imply a thickness H ⩾ 50 km. Then the flexures lead to an apparent Young's modulus an order of magnitude lower than that inferred from seismic wave velocities. It is suggested that the actual process at work is some kind of transient creep, which may be confused with elasticity only for non-decreasing stresses. The rise—trench problem is solved using this “pseudo-elastic” model." @default.
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- W1986585184 date "1974-10-01" @default.
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- W1986585184 title "Rheological properties of lithosphere" @default.
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- W1986585184 doi "https://doi.org/10.1016/0040-1951(74)90128-0" @default.
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