ROW: Numerical Modelling of Crystallization in Magma        Chambers
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Crystallization can occur at the boundaries of magma chambers or                within the body of the magma.  These processes can lead to                      convection in the liquid and  differentiation in liquid and solid               phases.  The basic physical mechanisms for crystallization at a                 side boundary have been demonstrated with laboratory experiemnts.               It is proposed 1) to model a binary system crystallizing from a                 side boundary and 2) to model crystallization within the magma.                 The combination will aid in our understanding of magmatic and                   volcanic processes.
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