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Metasomatism and the Chemical Transformation of Rock
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Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to
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Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to
Mantle Metasomatism
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Oceanic and Continental Lithosphere
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