Abstract.
It is proposed that the following normative pyroxene minerals be used: CaSiO3, MgSiO3, and FeSiO3 (with symbols “wo,” “en,” and “ hy,” respectively); and that the olivine molecule be given in terms of Mg2SiO4 and Fe2SiO4 (with symbols “ fo ” and “fa”). It is shown that these changes will improve the norm by bringing the ferro-magnesian minerals into a closer approach to natural conditions, by making it easier to survey their composition, and by rendering calculations simpler.
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Barth, T.F.W. Proposed Change in Calculation of Norms of Rocks.. Zeitschrift für Kristallographie, Mineralogie und Petrographie 42, 1–7 (1932). https://doi.org/10.1007/BF02938522
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DOI: https://doi.org/10.1007/BF02938522