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Titlebook: Chemical Transport in Metasomatic Processes; Harold C. Helgeson Book 1987 Springer Science+Business Media Dordrecht 1987 Mafic.chemistry.e

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Controls of the Chemical Composition of Geothermal Watersr with secondary minerals resulting from water-rock interaction. Simple calculations of the composition of water at equilibrium can be performed by using the concept of complete mineral association : the number of minerals is equal to the number of major inert elements in the solution. For each elem
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Lagrangian and Eulerian Representations of Metasomatic Alteration of Minerals on a continuum representation of porous media. The Eulerian method is an inherently transient description of advective and diffusive/dispersive transport referred to a reference frame that is fixed with respect to the rock mass. The Lagrangian method, applicable to flowing systems, is referred to a
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978-94-010-8280-8Springer Science+Business Media Dordrecht 1987
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