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Studies of Arc Volcanism and Mantle Behavior in Subduction Zones
Publié en 2015
Injection of 3-D hot plume blob develops localized and short-term increases in slab surface temperatures, consistent with the Abukuma adakite, Northeast Japan. 3-D mantle flow develops trough of the lowered slab surface temperatures implying along lowered slab surface temperatures, implying along-arc variations in arc variations in volcanism.
COMSOL Multiphysics using the CFD module allows easier modeling of the 3-D subduction experiments. However, export of the vector graphics (e.g., PDF or PS formats) is required for a better visualization for high-quality figures.
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- lee_presentation.pdf - 3.83MB