Fig. 6From: A multicomponent geothermometer for high-temperature basalt settingsComparison of an unspecific mineral set (a) with the developed basaltic set (b). The boxplot in the third column (c) is the result of the combination of the pH, aluminium concentration, and steam loss sensitivity analysis. All analyses are done separately under static conditions for the remaining parameters, and all best-fit parameters were combined afterwardsBack to article page