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McKechnie, C. L.; Annesley, I. R.; Ansdell, K. M. (2012) Medium- to Low-Pressure Pelitic Gneisses of Fraser Lakes Zone B, Wollaston Domain, Northern Saskatchewan, Canada: Mineral Compositions, Metamorphic P-T-T Path, and Implications for the Genesis of Radioactive Abyssal Granitic Pegmatites. The Canadian Mineralogist, 50 (6). 1669-1694 doi:10.3749/canmin.50.6.1669

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Reference TypeJournal (article/letter/editorial)
TitleMedium- to Low-Pressure Pelitic Gneisses of Fraser Lakes Zone B, Wollaston Domain, Northern Saskatchewan, Canada: Mineral Compositions, Metamorphic P-T-T Path, and Implications for the Genesis of Radioactive Abyssal Granitic Pegmatites
JournalThe Canadian Mineralogist
AuthorsMcKechnie, C. L.Author
Annesley, I. R.Author
Ansdell, K. M.Author
Year2012 (December 1)Volume50
Page(s)1669-1694Issue6
PublisherMineralogical Association of Canada
DOIdoi:10.3749/canmin.50.6.1669Search in ResearchGate
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Mindat Ref. ID65075Long-form Identifiermindat:1:5:65075:7
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Full ReferenceMcKechnie, C. L.; Annesley, I. R.; Ansdell, K. M. (2012) Medium- to Low-Pressure Pelitic Gneisses of Fraser Lakes Zone B, Wollaston Domain, Northern Saskatchewan, Canada: Mineral Compositions, Metamorphic P-T-T Path, and Implications for the Genesis of Radioactive Abyssal Granitic Pegmatites. The Canadian Mineralogist, 50 (6). 1669-1694 doi:10.3749/canmin.50.6.1669
Plain TextMcKechnie, C. L.; Annesley, I. R.; Ansdell, K. M. (2012) Medium- to Low-Pressure Pelitic Gneisses of Fraser Lakes Zone B, Wollaston Domain, Northern Saskatchewan, Canada: Mineral Compositions, Metamorphic P-T-T Path, and Implications for the Genesis of Radioactive Abyssal Granitic Pegmatites. The Canadian Mineralogist, 50 (6). 1669-1694 doi:10.3749/canmin.50.6.1669
In(2012, December) The Canadian Mineralogist Vol. 50 (6). Mineralogical Association of Canada

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Mckechnie, C. L.; Annesley, I. R.; Ansdell, K. M. (2012) Radioactive Abyssal Granitic Pegmatites and Leucogranites in the Wollaston Domain, Northern Saskatchewan, Canada: Mineral Compositions and Conditions of Emplacement in the Fraser Lakes Area. The Canadian Mineralogist, 50 (6). 1637-1667 doi:10.3749/canmin.50.6.1637
Pascal, Marjolaine, Ansdell, Kevin, Annesley, Irvine R., Kotzer, Tom, Jiricka, Dan (2016) Graphite-Bearing Pelitic Schists and Their Altered Equivalents In the Dufferin Lake Zone, South-Central Athabasca Basin, Saskatchewan: Constraints On Graphite Formation and Destruction, and Implications For Uranium Mineralization. The Canadian Mineralogist, 54 (6) 1459-1491 doi:10.3749/canmin.1600004
Alexandre, P., Uvarova, Y., Kyser, T. K. (2012) Origin of uranous and uranyl minerals at the Centennial deposit, Athabasca Basin, Northern Saskatchewan, Canada. The Canadian Mineralogist, 50 (3). 693-704 doi:10.3749/canmin.50.3.693
Novak, M., Skoda, R., Gadas, P., Krmicek, L., Cerny, P. (2012) Contrasting Origins of the Mixed (NYF + LCT) Signature in Granitic Pegmatites, with Examples from the Moldanubian Zone, Czech Republic. The Canadian Mineralogist, 50 (4) 1077-1094 doi:10.3749/canmin.50.4.1077
Galliski, M. A., London, D., Novák, M., Martin, R. F. (2012) Granitic pegmatites and their minerals: a second tribute to Petr Černý. The Canadian Mineralogist, 50 (6). 1441-1444 doi:10.3749/canmin.50.6.1441
Müller, Axel, Kearsley, A., Spratt, J., Seltmann, R. (2012) Petrogenetic implications of magmatic garnet in granitic pegmatites from Southern Norway. The Canadian Mineralogist, 50 (4) 1095-1115 doi:10.3749/canmin.50.4.1095
Galliski, M. A., London, D., Novak, M., Martin, R. F. (2012) Granitic Pegmatites and their Minerals: a Tribute to Petr Černý. The Canadian Mineralogist, 50 (4). 777-780 doi:10.3749/canmin.50.4.777
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Lupulescu, M. V.; Chiarenzelli, J. R.; Bailey, D. G. (2012) Mineralogy, Classification, and Tectonic Setting of the Granitic Pegmatites of New York State, Usa. The Canadian Mineralogist, 50 (6). 1713-1728 doi:10.3749/canmin.50.6.1713
London, D., Morgan, G. B., Paul, K. A., Guttery, B. M. (2012) Internal Evolution of Miarolitic Granitic Pegmatites at the Little Three Mine, Ramona, California, USA. The Canadian Mineralogist, 50 (4) 1025-1054 doi:10.3749/canmin.50.4.1025
 
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