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
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MATHER, J., ATHERTON, M. Stilpnomelane from the Dalradian. Nature 207, 971–972 (1965). https://doi.org/10.1038/207971a0
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DOI: https://doi.org/10.1038/207971a0
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