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Small amounts of H 2 O, on the order of tens to hundreds of parts per million, can significantly influence the physical properties of mantle rocks. Determining the H 2 O contents of nominally anhydrous minerals (NAMs) is one relatively common technique that has been applied to estimate mantle H 2 O contents. However, for many mantle NAMs, the relation between H 2 O activity and H 2 O content is not well known. Furthermore, certain mantle minerals may be prone to H 2 O loss during emplacement on Earth’s surface. The goal of this study is to apply mineral equilibria to estimate values of  a  H 2 O  in rocks that originated below the Moho.

Application of mineral equilibria to estimate fugacities of H 2 O, H 2 , and O 2 in mantle xenoliths from the southwestern U.S.A.