Location is approximate, estimate based on other nearby localities. | |
---|---|
Latitude & Longitude: | 37° North , 138° East (est.) |
Margin of Error: | ~133km |
W-Sn veins
Select Mineral List Type
Standard Detailed Strunz Dana Chemical ElementsDetailed Mineral List:
β Cassiterite Formula: SnO2 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Chalcopyrite Formula: CuFeS2 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Lillianite Formula: Pb3-2xAgxBi2+xS6 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Muscovite Formula: KAl2(AlSi3O10)(OH)2 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Muscovite var: Sericite Formula: KAl2(AlSi3O10)(OH)2 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Pyrite Formula: FeS2 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Pyrrhotite Formula: Fe7S8 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Quartz Formula: SiO2 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β Sphalerite Formula: ZnS Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
β 'Wolframite' Formula: (Fe2+)WO4 to (Mn2+)WO4 Reference: Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312. |
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | 'Chalcopyrite' | 2.CB.10a | CuFeS2 |
β | 'Lillianite' | 2.JB.40a | Pb3-2xAgxBi2+xS6 |
β | 'Pyrite' | 2.EB.05a | FeS2 |
β | 'Pyrrhotite' | 2.CC.10 | Fe7S8 |
β | Sphalerite | 2.CB.05a | ZnS |
Group 4 - Oxides and Hydroxides | |||
β | 'Cassiterite' | 4.DB.05 | SnO2 |
β | 'Quartz' | 4.DA.05 | SiO2 |
Group 9 - Silicates | |||
β | 'Muscovite' | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | var: Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
Unclassified Minerals, Rocks, etc. | |||
β | Wolframite | - | (Fe2+)WO4 to (Mn2+)WO4 |
List of minerals arranged by Dana 8th Edition classification
Group 2 - SULFIDES | |||
---|---|---|---|
AmXp, with m:p = 1:1 | |||
β | Pyrrhotite | 2.8.10.1 | Fe7S8 |
β | Sphalerite | 2.8.2.1 | ZnS |
AmBnXp, with (m+n):p = 1:1 | |||
β | Chalcopyrite | 2.9.1.1 | CuFeS2 |
AmBnXp, with (m+n):p = 1:2 | |||
β | Pyrite | 2.12.1.1 | FeS2 |
Group 3 - SULFOSALTS | |||
ΓΈ = 3 | |||
β | Lillianite | 3.4.15.1 | Pb3-2xAgxBi2+xS6 |
Group 4 - SIMPLE OXIDES | |||
AX2 | |||
β | Cassiterite | 4.4.1.5 | SnO2 |
Group 71 - PHYLLOSILICATES Sheets of Six-Membered Rings | |||
Sheets of 6-membered rings with 2:1 layers | |||
β | Muscovite | 71.2.2a.1 | KAl2(AlSi3O10)(OH)2 |
Group 75 - TECTOSILICATES Si Tetrahedral Frameworks | |||
Si Tetrahedral Frameworks - SiO2 with [4] coordinated Si | |||
β | Quartz | 75.1.3.1 | SiO2 |
Unclassified Minerals, Rocks, etc. | |||
β | Muscovite var: Sericite | - | KAl2(AlSi3O10)(OH)2 |
β | 'Wolframite' | - | (Fe2+)WO4 to (Mn2+)WO4 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Muscovite | KAl2(AlSi3O10)(OH)2 |
H | β Muscovite (var: Sericite) | KAl2(AlSi3O10)(OH)2 |
O | Oxygen | |
O | β Cassiterite | SnO2 |
O | β Muscovite | KAl2(AlSi3O10)(OH)2 |
O | β Quartz | SiO2 |
O | β Muscovite (var: Sericite) | KAl2(AlSi3O10)(OH)2 |
O | β Wolframite | (Fe2+)WO4 to (Mn2+)WO4 |
Al | Aluminium | |
Al | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | β Muscovite (var: Sericite) | KAl2(AlSi3O10)(OH)2 |
Si | Silicon | |
Si | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | β Quartz | SiO2 |
Si | β Muscovite (var: Sericite) | KAl2(AlSi3O10)(OH)2 |
S | Sulfur | |
S | β Chalcopyrite | CuFeS2 |
S | β Lillianite | Pb3-2xAgxBi2+xS6 |
S | β Pyrite | FeS2 |
S | β Pyrrhotite | Fe7S8 |
S | β Sphalerite | ZnS |
K | Potassium | |
K | β Muscovite | KAl2(AlSi3O10)(OH)2 |
K | β Muscovite (var: Sericite) | KAl2(AlSi3O10)(OH)2 |
Mn | Manganese | |
Mn | β Wolframite | (Fe2+)WO4 to (Mn2+)WO4 |
Fe | Iron | |
Fe | β Chalcopyrite | CuFeS2 |
Fe | β Pyrite | FeS2 |
Fe | β Pyrrhotite | Fe7S8 |
Fe | β Wolframite | (Fe2+)WO4 to (Mn2+)WO4 |
Cu | Copper | |
Cu | β Chalcopyrite | CuFeS2 |
Zn | Zinc | |
Zn | β Sphalerite | ZnS |
Ag | Silver | |
Ag | β Lillianite | Pb3-2xAgxBi2+xS6 |
Sn | Tin | |
Sn | β Cassiterite | SnO2 |
W | Tungsten | |
W | β Wolframite | (Fe2+)WO4 to (Mn2+)WO4 |
Pb | Lead | |
Pb | β Lillianite | Pb3-2xAgxBi2+xS6 |
Bi | Bismuth | |
Bi | β Lillianite | Pb3-2xAgxBi2+xS6 |
References
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Year (asc) Year (desc) Author (A-Z) Author (Z-A)Izumino, Y., & Nakashima, K. (2015). Bismuth minerals from the WβMoβSn deposits hosted in the Iwafune granitoids, Niigata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences, 110(6), 300-312.
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