Initial Water Compositions: Aqueous Alteration of Planetesimals

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Scientific paper

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Scientific paper

Oxygen isotope data for sulfate and carbonate minerals (alteration
products) point to an initial water-ice oxygen isotope composition
closer to that proposed by Clayton and Mayeda than to that of Young. The
implication being that water-ice does not lie on an extension of the
slope 1 CCAM line.

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