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Statements
1982
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viscous gravitational relaxation
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response of Maxwell models of planet to surface mass loads
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examination of factors which determine isostatic response
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free air gravity anomalies
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large-scale deglaciation events
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initial isostatic disequilibrium
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relative sea-level variations
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melting of Laurentide ice sheet
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estimate extent
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inference of mantle viscosity from isostatic adjustment data
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free air gravity data provide extremely high quality constraint upon viscosity of lower mantle
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