Unnamed (Ba-K-Fe Sulphide)
A material that is NOT an approved mineral species
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Formula:
Ba-K-Fe-S
K is a minor component.
Anthropogenic phase found in slag.
Possibly an K-bearing Fe-analogue of owensite.
A similar phase with the composition (FeBaCuK)S to (FeBaCuK)11S9 has been described by Eckstein et al. (1994) from a Ba- and Pb-rich slag in the Erzgebirge.
Possibly an K-bearing Fe-analogue of owensite.
A similar phase with the composition (FeBaCuK)S to (FeBaCuK)11S9 has been described by Eckstein et al. (1994) from a Ba- and Pb-rich slag in the Erzgebirge.
Unique Identifiers
Mindat ID:
43459
Long-form identifier:
mindat:1:1:43459:5
GUID
(UUID V4):
(UUID V4):
6ad44251-dc7f-48bf-b662-aeee82cc7b94
Chemistry of Unnamed (Ba-K-Fe Sulphide)
Mindat Formula:
Ba-K-Fe-S
K is a minor component.
K is a minor component.
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 Unnamed (Ba-K-Fe Sulphide)
mindat.org URL:
https://www.mindat.org/min-43459.html
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Please feel free to link to this page.
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References for Unnamed (Ba-K-Fe Sulphide)
Reference List:
Localities for Unnamed (Ba-K-Fe Sulphide)
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).
Struck out - Mineral was erroneously reported from this locality.
Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.
All localities listed without proper references should be considered as questionable.
Austria | |
| Kolitsch et al. (2013) |