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

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High Myopia Requires “High Attention” on fluid composition and fluid behaviour during the M2-metamorphism (mainly Naxos), and the M3-metamorphism (Serifos). Fluids during the M2 metamorphism on Naxos are mixed CO.-H.O fluids, with remarkably constant chemical and carbon isotopic composition, over the whole range of temperatures and lit

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Progress in Myopia Prevention and Control 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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18O/16O Evidence for Fluid-Rock Interaction in the Upper Mantle: Data from Ultramafic Nodules and K-with the equilibrium interpretation. The metasomatic .O-enrichments of the peridotites can be related to metasomatic enrichments in LIL elements and the development of amphibole and phlogopite. In recent studies of leucite-bearing lavas with .Sr/.Sr = 0.7102 to 0.7106 from the Alban Hills and M. Vul

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Metasomatism of the Continental Lithosphere: Simulation of Isotope and Element Abundance Behaviour atope systematics can be accounted for. Identification of fluid and solid end-members suggest for both volcanic provinces that fluids which presumably had their origin in the asthenosphere invaded, penetrated and metasomatised the lithospheric mantle and crustal material, which may be previously subd

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