Letter | Published:

Stilpnomelane from the Dalradian

Naturevolume 207pages971972 (1965) | Download Citation

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Abstract

STILPNOMELANE has been found as a constituent of the schists of many low-grade areas throughout the world1–3. In the Dalradian it has been described from the South-west Highland epidiorites4–6 but not from the greywackes and pelites of the Upper Dalradian, although it is mentioned as occurring in “the quartzo-feldspathic green schists of the Southern Dalradian” by Voll7.

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References

  1. 1

    Turner, F. J., and Hutton, C. O., Geol. Mag., 72, 1 (1935).

  2. 2

    Seki, Y., Jap. J. Geol. Geogr., 29, 233 (1958).

  3. 3

    Zen, E-an, Amer. Mineral., 45, 129 (1960).

  4. 4

    Wiseman, J. D. H., Quart. J. Geol. Soc. Lond., 90, 354 (1934).

  5. 5

    Hutton, C. O., Mineralog. Mag., 25, 172 (1938).

  6. 6

    Knill, J. L., Quart. J. Geol. Soc. Lond., 115, 339 (1959).

  7. 7

    Voll, G., L'pool. Manchr. Geol. J., 2, 503 (1959).

  8. 8

    Gruner, J. W., Amer. Mineral., 22, 912 (1937).

  9. 9

    Brindley, G. W., in X-ray Identification and Structures of Clay Minerals, edit. by Brindley, G. W., 13 (Mineralog. Soc., London, 1951).

  10. 10

    Gruner, J. W., Amer. Mineral., 29, 291 (1944).

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Affiliations

  1. Department of Geology, University of Liverpool

    • J. D. MATHER
    •  & M. P. ATHERTON

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https://doi.org/10.1038/207971a0

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