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Calcite Dolomite Line Marble Solution

Variation of oxygen isotope fractionation factors for CO 2 produced from carbonate by reaction with H 3 PO 4 at 100C as a function of the mole fraction of CaCO 3 for carbonates in the calcite CaCO 3magnesite MgCO 3 solidsolution.Line a is calculated using the relationship proposed by Rosenbaum and Sheppard 11 Eqn. .Line b represents simple solidsolution mixing

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