Carbon isotope fractionation between calcite, graphite and CO(2): An experimental study
The partitioning of stable carbon isotopes between calcite, graphite and carbon dioxide (CO2) was experimentally determined at temperature from 500-1200 degrees C. Attainment of carbon isotope equilibrium in CO2-calcite runs was proved by achieving the same fractionation from isotopically opposite d...
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Veröffentlicht in: | Contributions to mineralogy and petrology 1992-10, Vol.112 (1), p.35 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The partitioning of stable carbon isotopes between calcite, graphite and carbon dioxide (CO2) was experimentally determined at temperature from 500-1200 degrees C. Attainment of carbon isotope equilibrium in CO2-calcite runs was proved by achieving the same fractionation from isotopically opposite directions. |
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ISSN: | 0010-7999 1432-0967 |