Reference Type | Journal (article/letter/editorial) |
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Title | Hydrated copper oxalate, moolooite, in lichens |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Chisholm, J. E. | Author |
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Jones, G. C. | Author |
Purvis, O. W. | Author |
Year | 1987 (December) | Volume | 51 |
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Issue | 363 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_51/51-363-715.pdf+ |
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DOI | doi:10.1180/minmag.1987.051.363.12Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 1446 | Long-form Identifier | mindat:1:5:1446:9 |
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|
GUID | 0 |
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Full Reference | Chisholm, J. E., Jones, G. C., Purvis, O. W. (1987) Hydrated copper oxalate, moolooite, in lichens. Mineralogical Magazine, 51 (363) 715-718 doi:10.1180/minmag.1987.051.363.12 |
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Plain Text | Chisholm, J. E., Jones, G. C., Purvis, O. W. (1987) Hydrated copper oxalate, moolooite, in lichens. Mineralogical Magazine, 51 (363) 715-718 doi:10.1180/minmag.1987.051.363.12 |
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In | (1987, December) Mineralogical Magazine Vol. 51 (363) Mineralogical Society |
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Abstract/Notes | AbstractVivid blue inclusions in white whewellite or weddellite, occurring within the medulla of four lichen species growing on copper-bearing rocks, have been identified as the hydrated copper oxalate, moolooite, CuC2O4. nH2O (n ∼ 0.4–0.7), by infrared spectroscopy and X-ray powder diffraction. The mineral is believed to have been formed by reaction between oxalic acid secreted by the lichen and ground or surface water containing copper. |
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