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UM2002-03-O:AuHgPd

Valid as an unnamed mineral
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Formula:
~(Pd,Au,Hg)9O5
Compare, e.g., palladinite and UM1999-14-O:HPd. Corresponds to analysis no. 4 in Table 9 of the original description paper.

Co-described with UM2002-08-O:CuPd, UM2002-11-O:PdPtSe, UM2002-30-Se:BiPd, UM2002-37-Se:HgPd, and UM2002-38-Se:Pd.


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Unique IdentifiersHide

Mindat ID:
54306
Long-form identifier:
mindat:1:1:54306:0

Similar NamesHide

IMA Classification of UM2002-03-O:AuHgPdHide

IMA status notes:
Unnamed (probably valid)

Chemistry of UM2002-03-O:AuHgPdHide

Mindat Formula:
~(Pd,Au,Hg)9O5
Element Weights:
Element% weight
Pd92.292 %
O7.709 %

Calculated from ideal end-member formula.
Elements listed:
Au, Hg, O, Pd - 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 UM2002-03-O:AuHgPdHide

References for UM2002-03-O:AuHgPdHide

Localities for UM2002-03-O:AuHgPdHide

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.
Brazil
 
  • ParÃĄ
    • CurionÃģpolis
Cabral et al. (2002)
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