Description
Hello Nicolas,
Firstly, congratulations on this excellent program, it is simply easy to use and the new Julia web interface just adds to that. I am very impressed.
Not so much a problem, as a clarification here:
I am modelling a sub-solidus metabasite using the Green et al (2016) solution models, and I have set the bulk H2O content to '0', setting it in excess. I want to clarify if setting the H2O to 0 is MAGEMin's equivalent of excess, or is there some other way I may have overlooked (I haven't used the Matlab interface)?
Setting H2O to 0 in the bulk generates some higher P fields (10 - 12 kbar) containing two feldspars (ksp & ksp) indicating an extremely dry rock, and in some cases saturating the bulk (in a T-XH2O section) gives some fields with 2 hb phases.
Thanks again!