| 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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| Page(s) | 715-718 | 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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| Mindat Ref. ID | 1446 | Long-form Identifier | mindat:1:5:1446:9 |
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| GUID | e2d6e1f0-2c62-495a-b53a-4e490f749765 |
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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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