Mineral solubility and hydrous melting relations in the deep earth: Analysis of some binary A-H 2 O system pressure-temperature-composition topologies
Phase relations involving hydrous melting, volatile and mineral solubility and supercritical fluid phenomena at high pressure for mineral-H2O systems are generally not completely constrained by experimental data or adequately treated in thermodynamic models. Here we examine geometric relations in pressure (P)-temperature (T)-composition (X) topologies of simple hydrous A-H2O binaries, thus avoiding some of the pitfalls associated with other approaches. The relations between mineral solubility...[Show more]
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|Source:||American Journal of Science|
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