Abstract
The dark greyish interior of the meteorite consists of a dull ground-mass relieved by numerous black chondrules and spangles of a brassy mineral which is probably troilite (ferrous sulphide). The chondrules are very hard and compact and may quite easily be rubbed away from the friable ground-mass by the fingers.
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[Letter to the Editor]. Nature 127, 631 (1931). https://doi.org/10.1038/127631c0
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DOI: https://doi.org/10.1038/127631c0
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