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UM2004-25-O:FeHPt

Valid as an unnamed mineral
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Formula:
~PtFe3O5(OH) · 7H2O
Unique combination of elements, although identical to that in the co-described UM2004-29-OH:FePt. Also co-described with UM2004-22-O:CuFePdPt, UM2004-23-O:CuFePdPt, and UM2004-24-O:CuPd.


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Unique IdentifiersHide

Mindat ID:
54492
Long-form identifier:
mindat:1:1:54492:6

Similar NamesHide

IMA Classification of UM2004-25-O:FeHPtHide

IMA status notes:
Unnamed (probably valid)

Chemistry of UM2004-25-O:FeHPtHide

Mindat Formula:
~PtFe3O5(OH) · 7H2O
Element Weights:
Element% weight
O35.510 %
Pt33.306 %
Fe28.603 %
H2.581 %

Calculated from ideal end-member formula.
Elements listed:
Fe, H, O, Pt - 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 UM2004-25-O:FeHPtHide

References for UM2004-25-O:FeHPtHide

Localities for UM2004-25-O:FeHPtHide

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.
Spain
 
  • Extremadura
    • Badajoz
      • Monesterio
Ortega et al. (2004)
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