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• W2024494610 abstract "The 18O/16O and 13C/12C ratios have been determined for calcite samples of hydrothermal origin from the Ranchi area (India). The isotopic ratios are indicative of fractional crystallization as evidenced by the gradual increase of 18O/16O ratios with decreasing temperature of carbonate crystallization. However, there is no correlation between the 13C/12C and 18O/16O ratios. The absence of correlation may possibly be due to the exchange of the carbonate carbon with the surroundings." @default.
• W2024494610 created "2016-06-24" @default.
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• W2024494610 date "1970-04-01" @default.
• W2024494610 modified "2023-09-27" @default.
• W2024494610 title "Oxygen and carbon isotope ratios of some hydrothermal carbonates" @default.
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• W2024494610 doi "https://doi.org/10.1016/0020-7381(70)85022-7" @default.
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