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Predictive Mineralogy

Possible unrecorded species at Cu-arsenide occurrence, Sewen, Thann-Guebwiller, Haut-Rhin, Grand Est, France

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing speciesFormulaMatch %Due to recorded presence of
DomeykiteCu3As93.87%Koutekite (71.43 %), Kutinaite (50.00 %), Trigodomeykite (57.14 %)
ChalcopyriteCuFeS292.32%Koutekite (57.14 %), Kutinaite (50.00 %), Löllingite (64.20 %)
PyriteFeS292.01%Koutekite (52.38 %), Kutinaite (50.00 %), Löllingite (66.48 %)
QuartzSiO288.74%Koutekite (52.38 %), Löllingite (76.36 %)
ChalcociteCu2S87.50%Koutekite (66.67 %), Kutinaite (62.50 %)
CupriteCu2O83.33%Koutekite (66.67 %), Kutinaite (50.00 %)
CopperCu83.33%Koutekite (66.67 %), Kutinaite (50.00 %)
SilverAg78.57%Koutekite (57.14 %), Kutinaite (50.00 %)
CalciteCaCO376.67%Koutekite (52.38 %), Löllingite (51.02 %)
BorniteCu5FeS476.19%Koutekite (52.38 %), Kutinaite (50.00 %)
AzuriteCu3(CO3)2(OH)266.66%Koutekite (66.67 %)
MalachiteCu2(CO3)(OH)266.66%Koutekite (66.67 %)
ArsenopyriteFeAsS65.68%Löllingite (65.68 %)
GalenaPbS61.40%Kutinaite (50.00 %), Löllingite (53.52 %)
SphaleriteZnS47.63%Löllingite (59.55 %)

Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)


Predicting paragenetic modes of deposit

Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.

Paragenetic ModeScore
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Koutekite, Kutinaite, Trigodomeykite
100
34 : Complex granite pegmatites1
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)1