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- W2049304718 abstract "The depth below sea level of the Moho increases from about 15 km under Hawaii to about 20 km beneath Oahu. Computer simulation of the elastic flexure of the lithosphere due to the load of the Hawaiian archipelago reveals that the maximum downward displacement of the Moho should occur beneath Hawaii, not Oahu. It is concluded that the lithosphere in the Hawaiian area has a Maxwellian rheology, that the subsidence of the youngest island (Hawaii) may be largely due to elastic flexure, but that the additional 5 km subsidence of the 2.5 m.y. older Oahu represents viscous deformation of the lithosphere. The flexural rigidity of the lithosphere required to produce the subsidence of Hawaii by elastic flexure alone is 5 × 1030 dyne cm. The 5 km viscous settling of Oahu during 2.5 m.y. was then simulated utilizing an axisymmetric viscous finite-element computer program. The results indicate an effective lithospheric viscosity of approximately 3 × 1023 poise. This value is lower than most other estimates and may reflect the anomalous thermal regime in the Hawaiian region." @default.
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- W2049304718 date "1980-11-01" @default.
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- W2049304718 title "On the flexural rigidity and effective viscosity of the lithosphere in the Hawaiian area" @default.
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- W2049304718 doi "https://doi.org/10.1016/0040-1951(80)90208-5" @default.
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