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Adlakha, Erin E., Hattori, Keiko (2016) Paragenesis and Composition of Tourmaline Types Along the P2 Fault and Mcarthur River Uranium Deposit, Athabasca Basin, Canada. The Canadian Mineralogist, 54 (3) 661-679 doi:10.3749/canmin.1500057

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Reference TypeJournal (article/letter/editorial)
TitleParagenesis and Composition of Tourmaline Types Along the P2 Fault and Mcarthur River Uranium Deposit, Athabasca Basin, Canada
JournalThe Canadian Mineralogist
AuthorsAdlakha, Erin E.Author
Hattori, KeikoAuthor
Year2016 (May)Volume54
Issue3
PublisherMineralogical Association of Canada
DOIdoi:10.3749/canmin.1500057Search in ResearchGate
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Mindat Ref. ID65346Long-form Identifiermindat:1:5:65346:2
GUID0
Full ReferenceAdlakha, Erin E., Hattori, Keiko (2016) Paragenesis and Composition of Tourmaline Types Along the P2 Fault and Mcarthur River Uranium Deposit, Athabasca Basin, Canada. The Canadian Mineralogist, 54 (3) 661-679 doi:10.3749/canmin.1500057
Plain TextAdlakha, Erin E., Hattori, Keiko (2016) Paragenesis and Composition of Tourmaline Types Along the P2 Fault and Mcarthur River Uranium Deposit, Athabasca Basin, Canada. The Canadian Mineralogist, 54 (3) 661-679 doi:10.3749/canmin.1500057
In(2016, May) The Canadian Mineralogist Vol. 54 (3) Mineralogical Association of Canada

See Also

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Adlakha, E.E. & Hattori, K. (2016): Paragenesis and composition of tourmaline types along the P2 fault and Mcarthur River uranium deposit, Athabasca Basin, Canada. Canadian Mineralogist, 54, 661-679.
Adlakha, Erin E., Hattori, Keiko (2015) Compositional variation and timing of aluminum phosphate-sulfate minerals in the basement rocks along the P2 fault and in association with the McArthur River uranium deposit, Athabasca Basin, Saskatchewan, Canada. American Mineralogist, 100 (7) 1386-1399 doi:10.2138/am-2015-5069
Adlakha, E. E., & Hattori, K. (2015). Compositional variation and timing of aluminum phosphate-sulfate minerals in the basement rocks along the P2 fault and in association with the McArthur River uranium deposit, Athabasca Basin, Saskatchewan, Canada. American Mineralogist, 100(7), 1386-1399.
Adlakha, E., Hattori, K., Zaluski, G., Kotzer, T., & Potter, E. G. (2013). Alteration within the basement rocks associated with the P2 fault and the McArthur River uranium deposit, Athabasca Basin. Geological Survey of Canada Open File Report, 7462, 33.
Adlakha, Erin E., Hattori, Keiko, Davis, William J., Boucher, Brandon (2017) Characterizing fluids associated with the McArthur River U deposit, Canada, based on tourmaline trace element and stable (B, H) isotope compositions. Chemical Geology, 466. 417-435 doi:10.1016/j.chemgeo.2017.06.030
Reid, Kyle D., Ansdell, Kevin, Creighton, Steven, Potter, Eric G. (2016) Composition of Large Zoned Aluminum Phosphate Sulfate Minerals: Implications For Fluid Evolution In the Centennial Uranium Deposit Area, Athabasca Basin, Saskatchewan, Canada. The Canadian Mineralogist, 54 (5) 1205-1228 doi:10.3749/canmin.1500052
Adlakha, Erin E., Hattori, Keiko, Kerr, Mitchell J., Boucher, Brandon M. (2020) The origin of Ti-oxide minerals below and within the eastern Athabasca Basin, Canada. American Mineralogist, 105 (12) 1875-1888 doi:10.2138/am-2020-7235
Adlakha, E., Hattori, K. (2022) Thermotectonic events recorded by U-Pb geochronology and Zr-in-rutile thermometry of Ti oxides in basement rocks along the P2 fault, eastern Athabasca Basin, Saskatchewan, Canada. GSA Bulletin, 134 (3) 567-576 doi:10.1130/b35820.1
Alexandre, Paul (2021) Geochemistry of the Athabasca Basin, Saskatchewan, Canada, and the unconformity-related uranium deposits hosted by it. The Canadian Mineralogist, 59 (5) 847-868 doi:10.3749/canmin.1900002
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
Cerin, Daniele, Götze, Jens, Pan, Yuanming (2017) Radiation-Induced Damage In Quartz At the Arrow Uranium Deposit, Southwestern Athabasca Basin, Saskatchewan. The Canadian Mineralogist, 55 (3) 457-472 doi:10.3749/canmin.1700003
 
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