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

'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.
'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.
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.
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.
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.
'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.
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.
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.
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.
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.
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.
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
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.
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.
Gold
Formula: Au
Reference: http://www.mineralinfo.org/Fiches/canada/McArthur.htm
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.
'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.
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.
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.
'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.
'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.
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.
Molybdenite
Formula: MoS2
Reference: http://www.mineralinfo.org/Fiches/canada/McArthur.htm
'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.
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Reference: Geological Association of Canada (2014) Abstracts Fredericton Vol 37
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
Tellurium
Formula: Te
Reference: http://www.mineralinfo.org/Fiches/canada/McArthur.htm
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.
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.
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.
'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.
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
Gold1.AA.05Au
Graphite1.CB.05aC
Tellurium1.CC.10Te
Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Galena2.CD.10PbS
Molybdenite2.EA.30MoS2
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Corundum4.CB.05Al2O3
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Rutile4.DB.05TiO2
Uraninite4.DL.05UO2
var. Pitchblende4.DL.05UO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Siderite5.AB.05FeCO3
Group 8 - Phosphates, Arsenates and Vanadates
Arsenoflorencite-(Ce)8.BL.13CeAl3(AsO4)2(OH)6
Crandallite8.BL.10CaAl3(PO4)(PO3OH)(OH)6
Florencite-(Ce)8.BL.13CeAl3(PO4)2(OH)6
Svanbergite8.BL.05SrAl3(PO4)(SO4)(OH)6
Group 9 - Silicates
Clinochlore9.EC.55Mg5Al(AlSi3O10)(OH)8
Coffinite9.AD.30U(SiO4) · nH2O
Dickite9.ED.05Al2(Si2O5)(OH)4
Dravite9.CK.05NaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Kaolinite9.ED.05Al2(Si2O5)(OH)4
Magnesio-foitite9.CK.05◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Illite9.EC.15K0.65Al2.0[Al0.65Si3.35O10](OH)2
Oxy-dravite9.CK.05Na(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Oxy-schorl9.CK.05Na(Fe2+2Al)Al6(Si6O18)(BO3)3(OH)3O
Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Sudoite9.EC.55Mg2Al3(Si3Al)O10)(OH)8
Uranophane9.AK.15Ca(UO2)2(SiO3OH)2 · 5H2O
Zircon9.AD.30Zr(SiO4)
Unclassified Minerals, Rocks, etc.
'Alunite Supergroup'-AD3(XO4)2(OH)6
'Apatite'-Ca5(PO4)3(Cl/F/OH)
'Chlorite Group'-
'Gummite'-
'Leucoxene'-
'Limonite'-
'Monazite'-REE(PO4)
'Xenotime'-

List of minerals for each chemical element

HHydrogen
H SudoiteMg2Al3(Si3Al)O10)(OH)8
H DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
H CoffiniteU(SiO4) · nH2O
H Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
H SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
H Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
H ClinochloreMg5Al(AlSi3O10)(OH)8
H MuscoviteKAl2(AlSi3O10)(OH)2
H Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
H Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
H Florencite-(Ce)CeAl3(PO4)2(OH)6
H Alunite SupergroupAD3(XO4)2(OH)6
H KaoliniteAl2(Si2O5)(OH)4
H DickiteAl2(Si2O5)(OH)4
H UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
H ApatiteCa5(PO4)3(Cl/F/OH)
H Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
H CrandalliteCaAl3(PO4)(PO3OH)(OH)6
H SvanbergiteSrAl3(PO4)(SO4)(OH)6
BBoron
B DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
B Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
B SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
B Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
B Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
CCarbon
C GraphiteC
C CalciteCaCO3
C SideriteFeCO3
OOxygen
O SudoiteMg2Al3(Si3Al)O10)(OH)8
O DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
O Uraninite var. PitchblendeUO2
O UraniniteUO2
O QuartzSiO2
O HematiteFe2O3
O CoffiniteU(SiO4) · nH2O
O Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
O SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
O Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
O ClinochloreMg5Al(AlSi3O10)(OH)8
O MuscoviteKAl2(AlSi3O10)(OH)2
O Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
O Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
O Florencite-(Ce)CeAl3(PO4)2(OH)6
O Alunite SupergroupAD3(XO4)2(OH)6
O KaoliniteAl2(Si2O5)(OH)4
O CorundumAl2O3
O RutileTiO2
O MonaziteREE(PO4)
O DickiteAl2(Si2O5)(OH)4
O UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
O ZirconZr(SiO4)
O CalciteCaCO3
O SideriteFeCO3
O ApatiteCa5(PO4)3(Cl/F/OH)
O Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
O CrandalliteCaAl3(PO4)(PO3OH)(OH)6
O SvanbergiteSrAl3(PO4)(SO4)(OH)6
FFluorine
F ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Na DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Na SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Na Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Na Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
MgMagnesium
Mg SudoiteMg2Al3(Si3Al)O10)(OH)8
Mg DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Mg Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Mg ClinochloreMg5Al(AlSi3O10)(OH)8
Mg Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
AlAluminium
Al SudoiteMg2Al3(Si3Al)O10)(OH)8
Al DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Al Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Al SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Al Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Al ClinochloreMg5Al(AlSi3O10)(OH)8
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Al Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Al Florencite-(Ce)CeAl3(PO4)2(OH)6
Al KaoliniteAl2(Si2O5)(OH)4
Al CorundumAl2O3
Al DickiteAl2(Si2O5)(OH)4
Al Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
Al CrandalliteCaAl3(PO4)(PO3OH)(OH)6
Al SvanbergiteSrAl3(PO4)(SO4)(OH)6
SiSilicon
Si SudoiteMg2Al3(Si3Al)O10)(OH)8
Si DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Si QuartzSiO2
Si CoffiniteU(SiO4) · nH2O
Si Magnesio-foitite◻(Mg2Al)Al6(Si6O18)(BO3)3(OH)3(OH)
Si SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Si Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Si ClinochloreMg5Al(AlSi3O10)(OH)8
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Si Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Si KaoliniteAl2(Si2O5)(OH)4
Si DickiteAl2(Si2O5)(OH)4
Si UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Si ZirconZr(SiO4)
PPhosphorus
P Florencite-(Ce)CeAl3(PO4)2(OH)6
P MonaziteREE(PO4)
P ApatiteCa5(PO4)3(Cl/F/OH)
P CrandalliteCaAl3(PO4)(PO3OH)(OH)6
P SvanbergiteSrAl3(PO4)(SO4)(OH)6
SSulfur
S MolybdeniteMoS2
S GalenaPbS
S PyriteFeS2
S ChalcopyriteCuFeS2
S SvanbergiteSrAl3(PO4)(SO4)(OH)6
ClChlorine
Cl ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
K Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
K MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Ca UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Ca CalciteCaCO3
Ca ApatiteCa5(PO4)3(Cl/F/OH)
Ca CrandalliteCaAl3(PO4)(PO3OH)(OH)6
TiTitanium
Ti RutileTiO2
FeIron
Fe HematiteFe2O3
Fe SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Fe Oxy-schorlNa(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3O
Fe PyriteFeS2
Fe SideriteFeCO3
Fe ChalcopyriteCuFeS2
CuCopper
Cu ChalcopyriteCuFeS2
AsArsenic
As Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
SrStrontium
Sr SvanbergiteSrAl3(PO4)(SO4)(OH)6
ZrZirconium
Zr ZirconZr(SiO4)
MoMolybdenum
Mo MolybdeniteMoS2
TeTellurium
Te TelluriumTe
CeCerium
Ce Florencite-(Ce)CeAl3(PO4)2(OH)6
Ce Arsenoflorencite-(Ce)CeAl3(AsO4)2(OH)6
AuGold
Au GoldAu
PbLead
Pb GalenaPbS
UUranium
U Uraninite var. PitchblendeUO2
U UraniniteUO2
U CoffiniteU(SiO4) · nH2O
U 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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