Physics – Geophysics
Scientific paper
Sep 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993e%26psl.119..331w&link_type=abstract
Earth and Planetary Science Letters (ISSN 0012-821X), vol. 119, no. 3, p. 331-348
Physics
Geophysics
12
Earth (Planet), Earth Mantle, Geophysics, Ocean Models, Plates (Tectonics), Plumes, Tectonics, Fluid Flow, Fluid Mechanics, Heat Transmission, Viscosity
Scientific paper
This study addresses first-order aspects of the physics of continental lithosphere extension above mantle plumes, developing a testable model that predicts extension rates from flow parameters. Radial flow in the head of a plume causes a viscous force, and uplift over this head causes a buoyancy force, which both drive extension. The viscous force is roughly proportional to the plume's volume flux and, given my best estimates for flow parameters, predominated for the most vigorous plumes. Extension is opposed by a viscous force beyond the plume head, and its rate is thus affected by the dimensions of the plate on which this force acts. Extension rates are approximately 2 mm/yr above Yellowstone, less than approximately 1 mm/yr above Baikal, and approximately 0.7 mm/yr above the East African plume. Volume fluxes for all these plumes are approximately 50 cu m/s; the extension rates depend on plate dimensions.
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