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The ∼0.2 mm/yr uplift of Hawaiian islands Lanai and Molokai and Hawaiian swell topography pose important constraints on the structure and dynamics of mantle plumes. We have formulated 3-D models of mantle convection to investigate the effects of plume–plate interactions on surface vertical motions and swell topography. In our models, the controlling parameters are plume radius, excess plume temperature,...
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