Hi Brandon,
The base (P
o) is the initial pressure of melting and the top is the pressure at the base of the crust (P
c). The 1-D columns are for a column and the 2-D for a triangular melting regime, from which it is assumed that all the melt is extracted. The matrix streamlines are simplified (borrowing this image from an old post so ignore the coloured lines) and the melt ones aren't considered:
(https://content.screencast.com/users/magmasource/folders/topic41/media/032e4450-5071-4b10-8a49-0fa8fba40f1d/mor.jpg)
F
B is the mean extent of melting, where melting stops at P
c. The routine solves for P
c so that the pressure due to the overlying crust (assumed to have a density of 2.62 g.cm
-3) is P
c and the amount of extracted melt corresponds to F
B. See Asimow et al. (2001) (https://doi.org/10.1093/petrology/42.5.963) for more details, including equations.
Hope that helps. Sorry for delay.
Paula