The thermodynamic classification of basalts introduced by Carmichael et al. (1970) is based on aSiO2/melt vs. T°C data for the olivine/low-Ca pyroxene reaction. This classification is not consistent with geochemical classification schemes, and when aSiO2/melt data for a representative composition in the critical plane of silica undersaturation in the basalt tetrahedron are compared with the olivine/low-Ca pyroxene buffer curve, some rocks classified as alkali olivine basalts are shown to be tholeiitic basalts.

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First page of Silica activity and the classification of alkalic and tholeiitic basalts
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