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UM1986-52-Sb:AsPd

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Formula:
~Pd3(Sb,As)
author's formula: ~Pd11(Sb,As)4
Close to isomertieite.

The main component of a Pd-As-Sb spherule, about 200 microns in diameter, from an alluvial deposit. The spherule also contains 'UM1986-01-As:AuPdTe', 'UM1986-04-As:PdTe', and minor 'UM1986-66-Te:AsAuPd'.


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Unique IdentifiersHide

Mindat ID:
47858
Long-form identifier:
mindat:1:1:47858:0

Optical Data of UM1986-52-Sb:AsPdHide

Colour in reflected light:
pale yellow-white

Chemistry of UM1986-52-Sb:AsPdHide

Mindat Formula:
~Pd3(Sb,As)

author's formula: ~Pd11(Sb,As)4
Element Weights:
Element% weight
Pd72.391 %
Sb27.609 %

Calculated from ideal end-member formula.
Elements listed:
As, Pd, Sb - 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 UM1986-52-Sb:AsPdHide

References for UM1986-52-Sb:AsPdHide

Localities for UM1986-52-Sb:AsPdHide

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.

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.
Finland
 
  • Lapland
    • EnontekiÃķ
Vuorelainen et al. (1986) +1 other reference
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