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UM1982-09-S:AsCoFeNi

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Formula:
Co-Fe-Ni-As-S
Found as a component of rims of 30-micron-sized spherules, in association with cobaltite/gersdorffite partially replaced by bornite and digenite.

Chemically similar to 'UM1966-01-As:CoNiS', cobaltite and some other species.


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Unique IdentifiersHide

Mindat ID:
47645
Long-form identifier:
mindat:1:1:47645:8

Similar NamesHide

UM1989-01-AsS:CoFeNi(Ni,Fe,Co)AsS
UM1991-04-AsS:CoFeNi(Co,Ni,Fe,Cu)AsS

Chemistry of UM1982-09-S:AsCoFeNiHide

Mindat Formula:
Co-Fe-Ni-As-S
Element Weights:
Element% weight
As26.714 %
Co21.013 %
Ni20.928 %
Fe19.912 %
S11.433 %

Calculated from ideal end-member formula.
Elements listed:
As, Co, Fe, Ni, S - search for minerals with similar chemistry

Other InformationHide

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 UM1982-09-S:AsCoFeNiHide

References for UM1982-09-S:AsCoFeNiHide

Localities for UM1982-09-S:AsCoFeNiHide

Showing 1 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- 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.
Norway
 
  • Troms og Finnmark
    • Alta
Vokes et al. (1962) +1 other reference
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