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McArthur River Mine, Athabasca Basin, Saskatchewan, Canadai
Regional Level Types
McArthur River MineMine (Care and Maintenance)
Athabasca BasinBasin
SaskatchewanProvince
CanadaCountry

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Latitude & Longitude (WGS84):
57° 45' 45'' North , 105° 3' 6'' West
Latitude & Longitude (decimal):
Locality type:
Mine (Care and Maintenance) - last checked 2019
KΓΆppen climate type:


An U occurrence/mine opened in 1999.

World's largest known high-grade uranium deposit. 457 million lbs U3O8, average grade 23% U3O8.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


31 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

β“˜ 'Alunite Supergroup'
Formula: AD3(XO4)2(OH)6
Reference: 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.
β“˜ 'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
Reference: 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.
β“˜ Arsenoflorencite-(Ce)
Formula: CeAl3(AsO4)2(OH)6
Reference: 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.
β“˜ Calcite
Formula: CaCO3
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Chalcopyrite
Formula: CuFeS2
Reference: 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.
β“˜ 'Chlorite Group'
Reference: Geological Association of Canada (2014) Abstracts Fredericton Vol 37; 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.
β“˜ Clinochlore
Formula: Mg5Al(AlSi3O10)(OH)8
Reference: Geological Association of Canada (2014) Abstracts Fredericton Vol 37; 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.
β“˜ Coffinite
Formula: U(SiO4) · nH2O
Reference: http://www.mineralinfo.org/Fiches/canada/McArthur.htm; Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Corundum
Formula: Al2O3
Reference: 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.
β“˜ Crandallite
Formula: CaAl3(PO4)(PO3OH)(OH)6
Reference: 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.
β“˜ Dickite
Formula: Al2(Si2O5)(OH)4
Reference: 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.; Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Dravite
Formula: NaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Reference: www.laurentian.ca/geology/seminars/abstracts_f2001/Gammell.pdf.; Geological Association of Canada (2014) Abstracts Fredericton Vol 37
β“˜ Florencite-(Ce)
Formula: CeAl3(PO4)2(OH)6
Reference: 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.
β“˜ Galena
Formula: PbS
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Gold
Formula: Au
Reference: http://www.mineralinfo.org/Fiches/canada/McArthur.htm
β“˜ Graphite
Formula: C
Reference: 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.
β“˜ 'Gummite'
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Hematite
Formula: Fe2O3
Reference: www.laurentian.ca/geology/seminars/abstracts_f2001/Gammell.pdf.; 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.; Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.; 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.
β“˜ Kaolinite
Formula: Al2(Si2O5)(OH)4
Reference: 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, 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.
β“˜ 'Leucoxene'
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ 'Limonite'
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Magnesio-foitite
Formula: ◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Reference: Geological Association of Canada (2014) Abstracts Fredericton Vol 37; 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, 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.; Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.; 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.
β“˜ Molybdenite
Formula: MoS2
Reference: http://www.mineralinfo.org/Fiches/canada/McArthur.htm
β“˜ 'Monazite'
Formula: REE(PO4)
Reference: 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.
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Reference: Geological Association of Canada (2014) Abstracts Fredericton Vol 37
β“˜ Muscovite var. Illite
Formula: K0.65Al2.0[Al0.65Si3.35O10](OH)2
Reference: Geological Association of Canada (2014) Abstracts Fredericton Vol 37; 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, 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, 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.
β“˜ Oxy-dravite
Formula: Na(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Reference: 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.
β“˜ Oxy-schorl
Formula: Na(Fe2+2Al)Al6(Si6O18)(BO3)3(OH)3O
Reference: 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.
β“˜ Pyrite
Formula: FeS2
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.; 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.
β“˜ Quartz
Formula: SiO2
Reference: www.laurentian.ca/geology/seminars/abstracts_f2001/Gammell.pdf.; Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.; 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.
β“˜ Rutile
Formula: TiO2
Reference: 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.; Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Schorl
Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Reference: Geological Association of Canada (2014) Abstracts Fredericton Vol 37; 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.
β“˜ Siderite
Formula: FeCO3
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Sudoite
Formula: Mg2Al3(Si3Al)O10)(OH)8
Reference: www.laurentian.ca/geology/seminars/abstracts_f2001/Gammell.pdf.; Geological Association of Canada (2014) Abstracts Fredericton Vol 37; 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, 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, 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.
β“˜ Svanbergite
Formula: SrAl3(PO4)(SO4)(OH)6
Reference: 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.
β“˜ Tellurium
Formula: Te
Reference: http://www.mineralinfo.org/Fiches/canada/McArthur.htm
β“˜ Uraninite
Formula: UO2
Reference: www.laurentian.ca/geology/seminars/abstracts_f2001/Gammell.pdf; 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.
β“˜ Uraninite var. Pitchblende
Formula: UO2
Reference: www.laurentian.ca/geology/seminars/abstracts_f2001/Gammell.pdf.; Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ Uranophane
Formula: Ca(UO2)2(SiO3OH)2 · 5H2O
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
β“˜ 'Xenotime'
Reference: 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.
β“˜ Zircon
Formula: Zr(SiO4)
Reference: Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.; 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.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
β“˜Graphite1.CB.05aC
β“˜Tellurium1.CC.10Te
Group 2 - Sulphides and Sulfosalts
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Molybdenite2.EA.30MoS2
β“˜Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
β“˜Corundum4.CB.05Al2O3
β“˜Hematite4.CB.05Fe2O3
β“˜Quartz4.DA.05SiO2
β“˜Rutile4.DB.05TiO2
β“˜Uraninite4.DL.05UO2
β“˜var. Pitchblende4.DL.05UO2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
β“˜Siderite5.AB.05FeCO3
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Arsenoflorencite-(Ce)8.BL.13CeAl3(AsO4)2(OH)6
β“˜Crandallite8.BL.10CaAl3(PO4)(PO3OH)(OH)6
β“˜Florencite-(Ce)8.BL.13CeAl3(PO4)2(OH)6
β“˜Svanbergite8.BL.05SrAl3(PO4)(SO4)(OH)6
Group 9 - Silicates
β“˜Clinochlore9.EC.55Mg5Al(AlSi3O10)(OH)8
β“˜Coffinite9.AD.30U(SiO4) Β· nH2O
β“˜Dickite9.ED.05Al2(Si2O5)(OH)4
β“˜Dravite9.CK.05NaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Kaolinite9.ED.05Al2(Si2O5)(OH)4
β“˜Magnesio-foitite9.CK.05β—»(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Illite9.EC.15K0.65Al2.0[Al0.65Si3.35O10](OH)2
β“˜Oxy-dravite9.CK.05Na(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
β“˜Oxy-schorl9.CK.05Na(Fe2+2Al)Al6(Si6O18)(BO3)3(OH)3O
β“˜Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Sudoite9.EC.55Mg2Al3(Si3Al)O10)(OH)8
β“˜Uranophane9.AK.15Ca(UO2)2(SiO3OH)2 Β· 5H2O
β“˜Zircon9.AD.30Zr(SiO4)
Unclassified Minerals, Rocks, etc.
β“˜'Alunite Supergroup'-AD3(XO4)2(OH)6
β“˜'Apatite'-Ca5(PO4)3(Cl/F/OH)
β“˜'Chlorite Group'-
β“˜'Gummite'-
β“˜'Leucoxene'-
β“˜'Limonite'-
β“˜'Monazite'-REE(PO4)
β“˜'Xenotime'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ SudoiteMg2Al3(Si3Al)O10)(OH)8
Hβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ CoffiniteU(SiO4) · nH2O
Hβ“˜ Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Hβ“˜ ClinochloreMg5Al(AlSi3O10)(OH)8
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Hβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Hβ“˜ Florencite-(Ce)CeAl3(PO4)2(OH)6
Hβ“˜ Alunite SupergroupAD3(XO4)2(OH)6
Hβ“˜ KaoliniteAl2(Si2O5)(OH)4
Hβ“˜ DickiteAl2(Si2O5)(OH)4
Hβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Hβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
Hβ“˜ Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
Hβ“˜ CrandalliteCaAl3(PO4)(PO3OH)(OH)6
Hβ“˜ SvanbergiteSrAl3(PO4)(SO4)(OH)6
BBoron
Bβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Bβ“˜ Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Bβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Bβ“˜ Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Bβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
CCarbon
Cβ“˜ GraphiteC
Cβ“˜ CalciteCaCO3
Cβ“˜ SideriteFeCO3
OOxygen
Oβ“˜ SudoiteMg2Al3(Si3Al)O10)(OH)8
Oβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ Uraninite var. PitchblendeUO2
Oβ“˜ UraniniteUO2
Oβ“˜ QuartzSiO2
Oβ“˜ HematiteFe2O3
Oβ“˜ CoffiniteU(SiO4) · nH2O
Oβ“˜ Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Oβ“˜ ClinochloreMg5Al(AlSi3O10)(OH)8
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Oβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Oβ“˜ Florencite-(Ce)CeAl3(PO4)2(OH)6
Oβ“˜ Alunite SupergroupAD3(XO4)2(OH)6
Oβ“˜ KaoliniteAl2(Si2O5)(OH)4
Oβ“˜ CorundumAl2O3
Oβ“˜ RutileTiO2
Oβ“˜ MonaziteREE(PO4)
Oβ“˜ DickiteAl2(Si2O5)(OH)4
Oβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Oβ“˜ ZirconZr(SiO4)
Oβ“˜ CalciteCaCO3
Oβ“˜ SideriteFeCO3
Oβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
Oβ“˜ Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
Oβ“˜ CrandalliteCaAl3(PO4)(PO3OH)(OH)6
Oβ“˜ SvanbergiteSrAl3(PO4)(SO4)(OH)6
FFluorine
Fβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Naβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Naβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Naβ“˜ Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Naβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
MgMagnesium
Mgβ“˜ SudoiteMg2Al3(Si3Al)O10)(OH)8
Mgβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Mgβ“˜ Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Mgβ“˜ ClinochloreMg5Al(AlSi3O10)(OH)8
Mgβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
AlAluminium
Alβ“˜ SudoiteMg2Al3(Si3Al)O10)(OH)8
Alβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Alβ“˜ ClinochloreMg5Al(AlSi3O10)(OH)8
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Alβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Alβ“˜ Florencite-(Ce)CeAl3(PO4)2(OH)6
Alβ“˜ KaoliniteAl2(Si2O5)(OH)4
Alβ“˜ CorundumAl2O3
Alβ“˜ DickiteAl2(Si2O5)(OH)4
Alβ“˜ Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
Alβ“˜ CrandalliteCaAl3(PO4)(PO3OH)(OH)6
Alβ“˜ SvanbergiteSrAl3(PO4)(SO4)(OH)6
SiSilicon
Siβ“˜ SudoiteMg2Al3(Si3Al)O10)(OH)8
Siβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ QuartzSiO2
Siβ“˜ CoffiniteU(SiO4) · nH2O
Siβ“˜ Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Siβ“˜ ClinochloreMg5Al(AlSi3O10)(OH)8
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Siβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Siβ“˜ KaoliniteAl2(Si2O5)(OH)4
Siβ“˜ DickiteAl2(Si2O5)(OH)4
Siβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Siβ“˜ ZirconZr(SiO4)
PPhosphorus
Pβ“˜ Florencite-(Ce)CeAl3(PO4)2(OH)6
Pβ“˜ MonaziteREE(PO4)
Pβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
Pβ“˜ CrandalliteCaAl3(PO4)(PO3OH)(OH)6
Pβ“˜ SvanbergiteSrAl3(PO4)(SO4)(OH)6
SSulfur
Sβ“˜ MolybdeniteMoS2
Sβ“˜ GalenaPbS
Sβ“˜ PyriteFeS2
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ SvanbergiteSrAl3(PO4)(SO4)(OH)6
ClChlorine
Clβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
Kβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Caβ“˜ CalciteCaCO3
Caβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
Caβ“˜ CrandalliteCaAl3(PO4)(PO3OH)(OH)6
TiTitanium
Tiβ“˜ RutileTiO2
FeIron
Feβ“˜ HematiteFe2O3
Feβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Feβ“˜ Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Feβ“˜ PyriteFeS2
Feβ“˜ SideriteFeCO3
Feβ“˜ ChalcopyriteCuFeS2
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
AsArsenic
Asβ“˜ Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
SrStrontium
Srβ“˜ SvanbergiteSrAl3(PO4)(SO4)(OH)6
ZrZirconium
Zrβ“˜ ZirconZr(SiO4)
MoMolybdenum
Moβ“˜ MolybdeniteMoS2
TeTellurium
Teβ“˜ TelluriumTe
CeCerium
Ceβ“˜ Florencite-(Ce)CeAl3(PO4)2(OH)6
Ceβ“˜ Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
AuGold
Auβ“˜ GoldAu
PbLead
Pbβ“˜ GalenaPbS
UUranium
Uβ“˜ Uraninite var. PitchblendeUO2
Uβ“˜ UraniniteUO2
Uβ“˜ CoffiniteU(SiO4) · nH2O
Uβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O

References

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Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Marlatt, J., McGill, B., Matthews, R., Sopuck, V., & Pollock, G. (1992). The discovery of the McArthur River uranium deposit, Saskatchewan, Canada (No. IAEA-TECDOC--650).
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.
Ng, R., Alexandre, P., & Kyser, K. (2013). Mineralogical and geochemical evolution of the unconformity-related McArthur River Zone 4 orebody in the Athabasca Basin, Canada: implications of a silicified zone. Economic Geology, 108(7), 1657-1689.
Geological Association of Canada (2014), Abstracts Fredericton Volume 37.
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.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.

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