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MacMillan, Edeltraud, Ciobanu, Cristiana L., Ehrig, Kathy, Cook, Nigel J., Pring, Allan (2016) Replacement of Uraninite By BorniteViaCoupled Dissolution-Reprecipitation: Evidence From Texture and Microstructure. The Canadian Mineralogist, 54 (6) 1369-1383 doi:10.3749/canmin.1600031

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Reference TypeJournal (article/letter/editorial)
TitleReplacement of Uraninite By BorniteViaCoupled Dissolution-Reprecipitation: Evidence From Texture and Microstructure
JournalThe Canadian Mineralogist
AuthorsMacMillan, EdeltraudAuthor
Ciobanu, Cristiana L.Author
Ehrig, KathyAuthor
Cook, Nigel J.Author
Pring, AllanAuthor
Year2016 (November)Volume54
Issue6
PublisherMineralogical Association of Canada
DOIdoi:10.3749/canmin.1600031Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID65403Long-form Identifiermindat:1:5:65403:6
GUID0
Full ReferenceMacMillan, Edeltraud, Ciobanu, Cristiana L., Ehrig, Kathy, Cook, Nigel J., Pring, Allan (2016) Replacement of Uraninite By BorniteViaCoupled Dissolution-Reprecipitation: Evidence From Texture and Microstructure. The Canadian Mineralogist, 54 (6) 1369-1383 doi:10.3749/canmin.1600031
Plain TextMacMillan, Edeltraud, Ciobanu, Cristiana L., Ehrig, Kathy, Cook, Nigel J., Pring, Allan (2016) Replacement of Uraninite By BorniteViaCoupled Dissolution-Reprecipitation: Evidence From Texture and Microstructure. The Canadian Mineralogist, 54 (6) 1369-1383 doi:10.3749/canmin.1600031
In(2016, November) The Canadian Mineralogist Vol. 54 (6) Mineralogical Association of Canada

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Macmillan, Edeltraud, Cook, Nigel J., Ehrig, Kathy, Ciobanu, Cristiana L., Pring, Allan (2016) Uraninite from the Olympic Dam IOCG-U-Ag deposit: Linking textural and compositional variation to temporal evolution. American Mineralogist, 101 (6) 1295-1320 doi:10.2138/am-2016-5411
Macmillan, Edeltraud, Cook, Nigel J., Ehrig, Kathy, Pring, Allan (2017) Chemical and textural interpretation of late-stage coffinite and brannerite from the Olympic Dam IOCG-Ag-U deposit. Mineralogical Magazine, 81 (6) 1323-1366 doi:10.1180/minmag.2017.081.006
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