Closed jdannberg closed 3 weeks ago
This option was only useful because you would get large jumps in the grain size compositional field between upper and lower mantle, but now we can use particles instead.
Thank you! I've addressed your comment.
This option was only useful because you would get large jumps in the grain size compositional field between upper and lower mantle, but now we can use particles instead.
For new features/models or changes of existing features: