Dear Paula
I attempt simulate the magmatic differentiation of mantle-derived lamprophyre magmas. The fractionate phase is always olivine, which actually do not occur in the lamprophyres. Clinopyroxene is the major fractionate phase based on the petrography. The parameters I set are shown in the figure. The temperature and pressure were estimated via the clinopyroxene–liquid thermobarometer. The composition was from the whole rock, which is equilibrium with the clinopyroxene. I want to acquire a simulation that clinopyroxene is the only fractionate phase.
Could you help me find what the problem is at your convenience?
All the best
Gary
(https://www.helloimg.com/i/2025/01/07/677cbeb52faca.png)
(https://www.helloimg.com/i/2025/01/07/677cbeb575180.png)
Hi Gary,
Have you tried suppressing olivine?
Paula
Hi, Paula
I tried suppressing olivine. The easyMelts did not work. Then I increased the temperatures and decreased the pressures, then there was no fractionate phase. Next should I continue to adjust the conditions until the fractionate clinopyroxene occurs?
Many thanks!
Gary