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>Solubility and partitioning of noble gases in anorthite, diopside, forsterite, spinel, and synthetic basaltic melts: Implications for the origin and evolution of terrestrial planet atmospheres.
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Solubility and partitioning of noble gases in anorthite, diopside, forsterite, spinel, and synthetic basaltic melts: Implications for the origin and evolution of terrestrial planet atmospheres.