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A Model for the Solubility of Minerals in Saline Aqueous Fluids in the Crust and Upper Mantle
DownloadFall 2018
Quantifying and predicting the dissolution of minerals in complex (multicomponent) aqueous fluids across wide ranges of P-T space is critical for interpreting geologic processes that involve water-rock interactions in the Earth’s crust and upper mantle. Here, we define a new thermodynamic model...
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