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Cross Scale Modeling of Melt Migration

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MIMW02 - From the grain to the continuum: two phase dynamics of a partially molten, polycrystalline aggregate

The migration of melt over length scales of hundreds of kms takes place through grain edge tubules and films with typical dimensions of a few hundred nanometers to a few microns. The volume fraction, shape, and distribution of these tubules and films exert a strong influence on the effective physical properties, anisotropy, and the trajectory of melt migration in the mantle. In this talk, I will outline new techniques for modeling the microstructure in partially molten rocks,their influence on the effective physical properties, and the implications for large scale magma flow.

This talk is part of the Isaac Newton Institute Seminar Series series.

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