| Reference Type | Journal (article/letter/editorial) |
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| Title | Glushinskite, a naturally occurring magnesium oxalate |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Wilson, M. J. | Author |
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| Jones, D. | Author |
| Russell, J. D. | Author |
| Year | 1980 (September) | Volume | 43 |
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| Issue | 331 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_43/43-331-837.pdf+ |
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| DOI | doi:10.1180/minmag.1980.043.331.02Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 3153 | Long-form Identifier | mindat:1:5:3153:4 |
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| GUID | 0 |
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| Full Reference | Wilson, M. J., Jones, D., Russell, J. D. (1980) Glushinskite, a naturally occurring magnesium oxalate. Mineralogical Magazine, 43 (331) 837-840 doi:10.1180/minmag.1980.043.331.02 |
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| Plain Text | Wilson, M. J., Jones, D., Russell, J. D. (1980) Glushinskite, a naturally occurring magnesium oxalate. Mineralogical Magazine, 43 (331) 837-840 doi:10.1180/minmag.1980.043.331.02 |
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| In | (1980, September) Mineralogical Magazine Vol. 43 (331) Mineralogical Society |
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| Abstract/Notes | SummaryGlushinskite, 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. |
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