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Wisner South Deposit, Wisner Township, Sudbury District, Ontario, Canadai
Regional Level Types
Wisner South Deposit- not defined -
Wisner TownshipTownship
Sudbury DistrictDistrict
OntarioProvince
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Latitude & Longitude (WGS84):
46° North , 81° West (est.)
Estimate based on other nearby localities or region boundaries.
Margin of Error:
~7km


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Regions containing this locality

North America PlateTectonic Plate

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Standard Detailed Strunz Dana Chemical Elements

Mineral List


27 valid minerals.

Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Detailed Mineral List:

Acanthite
Formula: Ag2S
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Actinolite
Formula: ☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Aguilarite
Formula: Ag4SeS
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Albite
Formula: Na(AlSi3O8)
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Berryite
Formula: Cu3Ag2Pb3Bi7S16
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Bohdanowiczite
Formula: AgBiSe2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Cervelleite
Formula: Ag4TeS
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Chalcopyrite
Formula: CuFeS2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
'Chlorite Group'
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Empressite
Formula: AgTe
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Epidote
Formula: {Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
'Feldspar Group'
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Hematite
Formula: Fe2O3
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Hessite
Formula: Ag2Te
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Ilmenite
Formula: Fe2+TiO3
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
'K Feldspar'
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Kotulskite
Formula: Pd(Te,Bi)
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Lisiguangite
Formula: PtCuBiS3
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Magnetite
Formula: Fe2+Fe3+2O4
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Magnetite var: Mushketovite
Formula: Fe2+Fe3+2O4
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Malyshevite
Formula: PdCuBiS3
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Matildite
Formula: AgBiS2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Merenskyite
Formula: (Pd,Pt)(Te,Bi)2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Millerite
Formula: NiS
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Moncheite
Formula: (Pt,Pd)(Te,Bi)2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Polydymite
Formula: Ni2+Ni3+2S4
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Pyrite
Formula: FeS2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Quartz
Formula: SiO2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Rutile
Formula: TiO2
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Sobolevskite
Formula: Pd(Bi,Te)
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.
Titanite
Formula: CaTi(SiO4)O
Reference: Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Acanthite2.BA.35Ag2S
Aguilarite2.BA.55Ag4SeS
Berryite2.HB.20dCu3Ag2Pb3Bi7S16
Bohdanowiczite2.JA.20AgBiSe2
Cervelleite2.BA.60Ag4TeS
Chalcopyrite2.CB.10aCuFeS2
Empressite2.CB.80AgTe
Hessite2.BA.60Ag2Te
Kotulskite2.CC.05Pd(Te,Bi)
Lisiguangite2.GA.25PtCuBiS3
Malyshevite2.GA.25PdCuBiS3
Matildite2.JA.20AgBiS2
Merenskyite2.EA.20(Pd,Pt)(Te,Bi)2
Millerite2.CC.20NiS
Moncheite2.EA.20(Pt,Pd)(Te,Bi)2
Polydymite2.DA.05Ni2+Ni3+2S4
Pyrite2.EB.05aFeS2
Sobolevskite2.CC.05Pd(Bi,Te)
Group 4 - Oxides and Hydroxides
Hematite4.CB.05Fe2O3
Ilmenite4.CB.05Fe2+TiO3
Magnetite4.BB.05Fe2+Fe3+2O4
var: Mushketovite4.BB.05Fe2+Fe3+2O4
Quartz4.DA.05SiO2
Rutile4.DB.05TiO2
Group 9 - Silicates
Actinolite9.DE.10☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
Albite9.FA.35Na(AlSi3O8)
Epidote9.BG.05a{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Titanite9.AG.15CaTi(SiO4)O
Unclassified Minerals, Rocks, etc.
'Chlorite Group'-
'Feldspar Group'-
'K Feldspar'-

List of minerals arranged by Dana 8th Edition classification

Group 2 - SULFIDES
AmBnXp, with (m+n):p = 2:1
Acanthite2.4.1.1Ag2S
Aguilarite2.4.1.3Ag4SeS
Hessite2.4.2.1Ag2Te
AmXp, with m:p = 1:1
Empressite2.8.25.AgTe
Millerite2.8.16.1NiS
AmBnXp, with (m+n):p = 1:1
Chalcopyrite2.9.1.1CuFeS2
AmBnXp, with (m+n):p = 3:4
Polydymite2.10.1.7Ni2+Ni3+2S4
AmBnXp, with (m+n):p = 1:2
Merenskyite2.12.14.4(Pd,Pt)(Te,Bi)2
Moncheite2.12.14.3(Pt,Pd)(Te,Bi)2
Pyrite2.12.1.1FeS2
Group 3 - SULFOSALTS
ø = 3
Malyshevite3.4.4.3PdCuBiS3
2 < ø < 2.49
Berryite3.6.15.1Cu3Ag2Pb3Bi7S16
ø = 2
Bohdanowiczite3.7.1.2AgBiSe2
Matildite3.7.1.1AgBiS2
Group 4 - SIMPLE OXIDES
A2X3
Hematite4.3.1.2Fe2O3
Ilmenite4.3.5.1Fe2+TiO3
AX2
Rutile4.4.1.1TiO2
Group 7 - MULTIPLE OXIDES
AB2X4
Magnetite7.2.2.3Fe2+Fe3+2O4
Group 52 - NESOSILICATES Insular SiO4 Groups and O,OH,F,H2O
Insular SiO4 Groups and O, OH, F, and H2O with cations in [6] and/or >[6] coordination
Titanite52.4.3.1CaTi(SiO4)O
Group 58 - SOROSILICATES Insular, Mixed, Single, and Larger Tetrahedral Groups
Insular, Mixed, Single, and Larger Tetrahedral Groups with cations in [6] and higher coordination; single and double groups (n = 1, 2)
Epidote58.2.1a.7{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Group 75 - TECTOSILICATES Si Tetrahedral Frameworks
Si Tetrahedral Frameworks - SiO2 with [4] coordinated Si
Quartz75.1.3.1SiO2
Group 76 - TECTOSILICATES Al-Si Framework
Al-Si Framework with Al-Si frameworks
Albite76.1.3.1Na(AlSi3O8)
Unclassified Minerals, Mixtures, etc.
Actinolite-☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
Cervelleite-Ag4TeS
'Chlorite Group'-
'Feldspar Group'-
'K Feldspar'-
Kotulskite-Pd(Te,Bi)
Lisiguangite-PtCuBiS3
Magnetite
var: Mushketovite
-Fe2+Fe3+2O4
Sobolevskite-Pd(Bi,Te)

List of minerals for each chemical element

HHydrogen
H Actinolite☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
H Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
OOxygen
O Actinolite☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
O AlbiteNa(AlSi3O8)
O Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
O HematiteFe2O3
O IlmeniteFe2+TiO3
O MagnetiteFe2+Fe23+O4
O Magnetite (var: Mushketovite)Fe2+Fe23+O4
O QuartzSiO2
O RutileTiO2
O TitaniteCaTi(SiO4)O
NaSodium
Na AlbiteNa(AlSi3O8)
MgMagnesium
Mg Actinolite☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
AlAluminium
Al AlbiteNa(AlSi3O8)
Al Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
SiSilicon
Si Actinolite☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
Si AlbiteNa(AlSi3O8)
Si Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Si QuartzSiO2
Si TitaniteCaTi(SiO4)O
SSulfur
S ChalcopyriteCuFeS2
S MilleriteNiS
S PolydymiteNi2+Ni23+S4
S PyriteFeS2
S AcanthiteAg2S
S AguilariteAg4SeS
S BerryiteCu3Ag2Pb3Bi7S16
S CervelleiteAg4TeS
S LisiguangitePtCuBiS3
S MalyshevitePdCuBiS3
S MatilditeAgBiS2
CaCalcium
Ca Actinolite☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
Ca Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Ca TitaniteCaTi(SiO4)O
TiTitanium
Ti IlmeniteFe2+TiO3
Ti RutileTiO2
Ti TitaniteCaTi(SiO4)O
FeIron
Fe Actinolite☐{Ca2}{Mg4.5-2.5Fe0.5-2.5}(Si8O22)(OH)2
Fe ChalcopyriteCuFeS2
Fe Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Fe HematiteFe2O3
Fe IlmeniteFe2+TiO3
Fe MagnetiteFe2+Fe23+O4
Fe Magnetite (var: Mushketovite)Fe2+Fe23+O4
Fe PyriteFeS2
NiNickel
Ni MilleriteNiS
Ni PolydymiteNi2+Ni23+S4
CuCopper
Cu ChalcopyriteCuFeS2
Cu BerryiteCu3Ag2Pb3Bi7S16
Cu LisiguangitePtCuBiS3
Cu MalyshevitePdCuBiS3
SeSelenium
Se AguilariteAg4SeS
Se BohdanowicziteAgBiSe2
PdPalladium
Pd KotulskitePd(Te,Bi)
Pd MalyshevitePdCuBiS3
Pd Merenskyite(Pd,Pt)(Te,Bi)2
Pd Moncheite(Pt,Pd)(Te,Bi)2
Pd SobolevskitePd(Bi,Te)
AgSilver
Ag AcanthiteAg2S
Ag AguilariteAg4SeS
Ag BerryiteCu3Ag2Pb3Bi7S16
Ag BohdanowicziteAgBiSe2
Ag CervelleiteAg4TeS
Ag EmpressiteAgTe
Ag HessiteAg2Te
Ag MatilditeAgBiS2
TeTellurium
Te CervelleiteAg4TeS
Te EmpressiteAgTe
Te HessiteAg2Te
Te KotulskitePd(Te,Bi)
Te Merenskyite(Pd,Pt)(Te,Bi)2
Te Moncheite(Pt,Pd)(Te,Bi)2
Te SobolevskitePd(Bi,Te)
PtPlatinum
Pt LisiguangitePtCuBiS3
Pt Moncheite(Pt,Pd)(Te,Bi)2
PbLead
Pb BerryiteCu3Ag2Pb3Bi7S16
BiBismuth
Bi BerryiteCu3Ag2Pb3Bi7S16
Bi BohdanowicziteAgBiSe2
Bi KotulskitePd(Te,Bi)
Bi LisiguangitePtCuBiS3
Bi MalyshevitePdCuBiS3
Bi MatilditeAgBiS2
Bi Moncheite(Pt,Pd)(Te,Bi)2
Bi SobolevskitePd(Bi,Te)

References

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Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78.


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