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Dimorphic And Trimorphic In Minerals

Numerous secondary mineral fluid reactions have been shown to occur in crystalline rock environments Bucher and Stober, 2000.As mentioned previously, reactions in ultramafic and mafic rocks can have considerable control on pH, carbonate precipitation, and most likely the accumulation of excess H 2 gas Barnes and ONeil, 1971 Sherwood Lollar et al., 1993b.

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