Wisner South Deposit, Wisner Township, Greater Sudbury, Ontario, Canada (original) (raw)

ⓘ Acanthite

Formula: Ag2S

References:

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

References:

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

References:

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)

References:

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

References:

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

References:

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

References:

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

References:

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'

References:

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

References:

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: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)

References:

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'

References:

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

References:

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

References:

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

References:

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'

References:

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)2-x (x ≈ 0.4)

References:

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

References:

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

References:

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

References:

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

References:

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

References:

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: PdTe2

References:

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

References:

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(Te,Bi)2

References:

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

References:

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

References:

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

References:

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

References:

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: PdBi

References:

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

References:

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.