Physics
Scientific paper
Feb 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993georl..20..225f&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 20, no. 3, p. 225-228.
Physics
48
Earth Mantle, Free Convection, Hydrostatics, Seismology, Tomography, Topography, Geoids, Viscous Flow
Scientific paper
The very long wavelength dynamic topography at the earth's surface, estimated by isostatic reduction of the observed topography, is shown to be in good agreement with the topography predicted by a model of viscous flow in the mantle. This flow model was previously derived by independent consideration of the observed nonhydrostatic geoid and is based upon a recent model of large-scale seismic shear velocity heterogeneity in the mantle. Our estimate of the long wavelength dynamic surface topography reveals significant depressions of the continental shields relative to their hydrostatic reference positions.
Dziewonski Adam M.
Forte Alessandro M.
Peltier Richard W.
Woodward Robert L.
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