Kohlstedt [1992] provides a comprehensive synthesis of experimental
constraints on
the structure, rheology, and permeability of partially molten rocks.
Riley and
Kohlstedt [1991] presented experimental data that suggests that partially
molten material
in which the matrix is dominated by olivine will be very permeable even at
very low melt
fractions. Waff and Faul [1992] explored the effects of crystalline
anisotropy on
the distribution of melt in partially molten peridotite, and Daines and
Kohlstedt
[1994] showed that a transition from porous to channelized flow occurs due
to melt/rock
reaction during melt migration.