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Get Free AccessSummary Glushinskite, a dihydrate of magnesium oxalate, occurs at the lichen/rock interface on serpentinite colonized by Lecanora atra at Mill of Johnston, near Insch in north-east Scotland. It is found in a creamy white layer intermingled with the hyphae of the lichen fungus. It consists of crystals mainly 2 to 5 µm in size showing a distorted pyramidal form, often with curved and striated faces. X-ray, infrared, and chemical data are given.
M. J. Wilson, Davey L Jones, James Russell (1980). Glushinskite, a naturally occurring magnesium oxalate. Mineralogical Magazine, 43(331), pp. 837-840, DOI: 10.1180/minmag.1980.043.331.02.
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Type
Article
Year
1980
Authors
3
Datasets
0
Total Files
0
Language
English
Journal
Mineralogical Magazine
DOI
10.1180/minmag.1980.043.331.02
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