Rise and Deflection of mantle plume rails
Experimental observations by Kerr and Mériaux (2004) of the deflection of thermal plume tails by an imposed background shear are reanalyzed using a corrected velocity profile. The deflected plumes are found to be accurately described by a constant vertic
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|Source:||Geochemistry, Geophysics, Geosystems. G3|
|01_Kerr_Rise_and_Deflection_of_mantle_2008.pdf||927.69 kB||Adobe PDF||Request a copy|
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