A T–X pseudosection in KFMASH (+mu+q+H2O), for a composition line along which FeO:MgO varies, with X = FeO/(FeO+MgO)
Originally uploaded in Integrating Research and Education:Teaching Phase Equilibria.
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Mar30 07
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- THERMOCALC
https://serc.carleton.edu/research_education/equilibria/thermocalc.html
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