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Laboratory-Scale Simulation of Spiral Plumes in the Mantle
Published 3 Jul 2012 in physics.flu-dyn | (1207.0717v1)
Abstract: On the basis of laboratory simulation a mechanism is established for the formation of the upper mantle convection spiral plumes from a hot point in the presence of a roll-type large-scale convective flow. The observed plume has horizontal sections near the upper limit, which may lead to the formation of chains of volcanic islands.
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