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Evolution of the Oceans and the Origin of Fine-Grained Dolomites

Naturevolume 207pages930933 (1965) | Download Citation

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References

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    For reviews of the dolomite problem, see Sonnenfeld, P., Bull. Canad. Petrol. Geol., 12, 101 (1964), Fairbridge, R. W., in Regional Aspects of Carbonate Deposition, Soc. Econ. Paleo. Mineral. Spec. Pub. 5, 125 (1957), and Ingerson, E., Geochim. Cosmochim. Acta, 26, 817 (1962).

  2. 2

    Epstein, S., Graf, D. L., and Degens, E. T., in Isotopic and Cosmic Chemistry, 169 (North Holland Publishing Co., Amsterdam, 1963).

  3. 3

    Clayton, R. N., and Epstein, S., J. Geology, 66, 351 (1958).

  4. 4

    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).

  5. 5

    Silverman, S. R., Geochim. Cosmochim. Acta, 2, 26 (1951).

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    Degens, E. T., Neues Jahrb. Geol. Paläeontol., Monatsh., No. 4, 180 (1959).

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    Weber, J. N., Ann. Meet. Geol. Soc. Amer., Preprints (Abst.), 218 (1964), Geokhimiya, No. 6, 674 (1965).

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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).

  9. 9

    Degens, E. T., and Epstein, S., Bull. Amer. Assoc. Petrol. Geol., 46, 534 (1962).

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    Keith, M. L., and Weber, J. N., Geochim. Cosmochim. Acta, 28, 1787 (1964).

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    Degens, E. T., and Epstein, S., Geochim. Cosmochim. Acta, 38, 23 (1964).

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    Weber, J. N., Science, 145, 1303 (1964).

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    Weber, J. N., P. 972 of this issue of Nature.

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  1. Department of Geochemistry and Mineralogy, Pennsylvania State University, Pennsylvania

    • PROF. JON N. WEBER

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https://doi.org/10.1038/207930a0

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