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UM1992-06-E:AgPd

Valid as an unnamed mineral
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Formula:
AgPd
Two angular grains found, 5 x 15 microns in size. They existed in a void of an Fe oxide nodule comprising mainly goethite and hematite. The nodule comes from a lateritic Au deposit.


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Unique IdentifiersHide

Mindat ID:
52131
Long-form identifier:
mindat:1:1:52131:4

Similar NamesHide

UM1973-05-Bi:AgPd(Ag,Pd)2Bi
UM1973-23-Te:AgPd(Pd,Ag)4Te
UM1986-17-E:CuPtPtCu3
UM1991-25-Te:AgPdValid as an unnamed mineralPd6AgTe4
UM1992-10-E:CuPtValid as an unnamed mineralPtCu5
UM1992-22-S:AgPdValid as an unnamed mineralPd2AgS2
UM1995-18-O:CuPdA synonym of Palladinite
UM1996-05-E:AgAuPdValid as an unnamed mineralAu6AgPd
UM1996-06-E:AuCuPdValid as an unnamed mineralAu4PdCu
UM1996-07-E:AuCuPdValid as an unnamed mineralAu7CuPd
UM1996-09-E:CuPtValid as an unnamed mineralPt2Cu
UM1996-10-E:CuPtValid as an unnamed mineralPt5Cu2
UM1996-11-E:CuPtA synonym of Kitagohaite
UM1999-08-E:AuHgPdValid as an unnamed mineralPd0.7Au0.3Hg0.1
UM1999-09-E:AuPdValid as an unnamed mineralPd3Au2
UM2000-04-E:AuCuPdValid as an unnamed mineralAu0.69Pd0.23Cu0.08
UM2002-03-O:AuHgPdValid as an unnamed mineral~(Pd,Au,Hg)9O5
UM2002-08-O:CuPdValid as an unnamed mineral~Pd4Cu5O9
UM2004-08-E:AuCuPdValid as an unnamed mineralCu2PdAu
UM2004-24-O:CuPd~PdCu2O3
UM2008-11-E:AuPdValid as an unnamed mineralAu3Pd
UM2010-08-S:AgPdInvalid as an unnamed mineral(Pd,Ag)4S

IMA Classification of UM1992-06-E:AgPdHide

IMA status notes:
Unnamed (probably valid)

Chemistry of UM1992-06-E:AgPdHide

Mindat Formula:
AgPd
Element Weights:
Element% weight
Ag50.338 %
Pd49.662 %

Calculated from ideal end-member formula.

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 UM1992-06-E:AgPdHide

References for UM1992-06-E:AgPdHide

Localities for UM1992-06-E:AgPdHide

Showing 1 localities.

ⓘ - 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
 
Zang et al. (1992) +1 other reference
 
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