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Minerals of the amphibole group are found in igneous rocks on Earth and other rocky bodies. Since the O(3) site of amphibole can contain OH, O 2- , F, and Cl, amphibole composition provides important information about water and halogen contents, oxidation state, and other features of its formation and alteration environments. However, the complexity of amphibole crystal chemistry means this information is difficult to extract. Furthermore, it has been regular practice in the era of the electron microprobe to neglect H and Fe 3+  analyses for amphibole, critically reducing the amount of information available in amphibole analyses in the literature.

Quantitative models linking igneous amphibole composition with magma Cl and OH content