UM1995-34-SO:Fe
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Formula:
FeS2O3
Quite often among carbonate-hosted Zn-Pb(Fe) ore mineralization in Upper Silesia, Poland (e.g., Pieczonka, 2010). The material coded as the "UM" species comes from the Amelia mine, Wisconsin, USA.
One of a few mixed/intermediate-valence Fe-S natural compounds known. In the carbonate-hosted ore deposits these compounds occur as subsulphites (see Unnamed (Fe Subsulphite)), sulphites (Unnamed (Fe Sulphite), Unnamed (Zn Sulphite)), pyrosulphites (Unnamed (Fe Pyrosulphite)), sulphoxylanes (Unnamed (Fe Sulphoxylane)), thiosulphates (compare Unnamed (Fe Thiosulphate II) and Unnamed (Pb Thiosulphate)).
These compounds are generally banded/radial/fibrous/spherulitic in form and have lowered reflectivity with growing sulphur valence. Compare also Unnamed (Fe Oxysulphide).
Upper Silesia, Poland: Botryoidal, with outer rim often recrystallized to pyrite and marcasite. Also as fibrous, syntiaxial intergrowths with sulfides and sulfates. May be oxygen-deficient.
Wisconsin, USA: As a mixture with pyrite-marcasite, that forms black patches. Analysis given in the Chemistry section concerns a homogenous area 40-50 microns in size. Determined thanks to the fact, that the valence state of S is related to wavelength shifts in the peaks for S in the electron microprobe analysis (EPMA).
Compare viaeneite; albertiniite (a sulphite).
One of a few mixed/intermediate-valence Fe-S natural compounds known. In the carbonate-hosted ore deposits these compounds occur as subsulphites (see Unnamed (Fe Subsulphite)), sulphites (Unnamed (Fe Sulphite), Unnamed (Zn Sulphite)), pyrosulphites (Unnamed (Fe Pyrosulphite)), sulphoxylanes (Unnamed (Fe Sulphoxylane)), thiosulphates (compare Unnamed (Fe Thiosulphate II) and Unnamed (Pb Thiosulphate)).
These compounds are generally banded/radial/fibrous/spherulitic in form and have lowered reflectivity with growing sulphur valence. Compare also Unnamed (Fe Oxysulphide).
Upper Silesia, Poland: Botryoidal, with outer rim often recrystallized to pyrite and marcasite. Also as fibrous, syntiaxial intergrowths with sulfides and sulfates. May be oxygen-deficient.
Wisconsin, USA: As a mixture with pyrite-marcasite, that forms black patches. Analysis given in the Chemistry section concerns a homogenous area 40-50 microns in size. Determined thanks to the fact, that the valence state of S is related to wavelength shifts in the peaks for S in the electron microprobe analysis (EPMA).
Compare viaeneite; albertiniite (a sulphite).
Unique Identifiers
Mindat ID:
47350
Long-form identifier:
mindat:1:1:47350:3
Similar Names
| UM1949-01-PO:Fe | FePO4 | |
| UM1958-02-PO:Fe | Fe-P-O | |
| UM1970-17-PO:Fe | Fe4(PO4)3 | |
| UM1971-02-AsO:Fe | Fe-As-O | |
| UM1979-03-AsO:Fe | FeAsO4 ? | |
| UM1979-04-AsO:Fe | FeAsO4 ? | |
| UM1981-12-S:CoFe | ~(Co,Fe)4S3 | |
| UM1988-20-SO:FeH | Fe2.67(SO4)2.14H2O | |
| UM1991-20-Si:Fe | Fe5Si2 | |
| UM1997-14-AsO:FeH | Fe-As-O-H | |
| UM1997-15-AsO:FeH | Fe-As-O-H | |
| UM1997-43-S:Fe | FeS3 | |
| UM2000-60-Si:Fe | Fe3Si7 | |
| UM2007-30-S:Fe | Fe3S2 |
Optical Data of UM1995-34-SO:Fe
Bireflectance:
yes
Chemistry of UM1995-34-SO:Fe
Mindat Formula:
FeS2O3
Element Weights:
Elements listed:
Other Information
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for UM1995-34-SO:Fe
mindat.org URL:
https://www.mindat.org/min-47350.html
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References for UM1995-34-SO:Fe
Reference List:
Kucha, H., Viaene, W. (1993) Compounds with mixed and intermediate sulfur valences as precursors of banded sulfides in carbonate-hosted Zn-Pb deposits in Belgium and Poland. Mineralium Deposita, 28 (1). 13-21 doi:10.1007/bf00199005
Localities for UM1995-34-SO:Fe
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
All localities listed without proper references should be considered as questionable.
Belgium | |
| Kucha et al. (1993) |
Poland | |
| Kucha H. |
| Pieczonka (2010) |
USA | |
| Kucha et al. (1995) +1 other reference |
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