References
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Because low temperature isotopic equilibrium has not been demonstrated experimentally at this time, 18O enrichment in dolomite is contended; see Friedman, I., and Hall, W. E., J. Geology, 71, 238 (1963).
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See Rubey, W. W., in The Origin and Evolution of Atmospheres and Oceans, 1 (John Wiley and Sons, New York, 1964).
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WEBER, J. Evolution of the Oceans and the Origin of Fine-Grained Dolomites. Nature 207, 930–933 (1965). https://doi.org/10.1038/207930a0
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DOI: https://doi.org/10.1038/207930a0
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