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Predictive Mineralogy

Possible unrecorded species at Pont Napoléon Quarry (Rioumajou Quarry), Rioumajou Valley, Luz-Saint-Sauveur, Argelès-Gazost, Hautes-Pyrénées, Occitanie, 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
QuartzSiO299.99%Calcite (62.43 %), Cobaltite (70.11 %), Erythrite (69.80 %), Graphite (54.90 %), Nickeline (58.64 %), Nickelskutterudite (74.76 %), Orthoclase (76.14 %), Prehnite (64.07 %), Pyrrhotite (67.51 %)
PyriteFeS299.91%Calcite (51.16 %), Cobaltite (78.87 %), Erythrite (64.88 %), Nickeline (66.71 %), Nickelskutterudite (66.02 %), Pyrrhotite (80.12 %)
ChalcopyriteCuFeS279.92%Cobaltite (85.76 %), Erythrite (69.91 %), Nickeline (72.98 %), Nickelskutterudite (65.05 %), Pyrrhotite (76.22 %)
SphaleriteZnS78.76%Cobaltite (60.74 %), Erythrite (50.44 %), Nickeline (53.48 %), Nickelskutterudite (61.65 %), Pyrrhotite (55.40 %)
GalenaPbS77.11%Cobaltite (57.74 %), Erythrite (53.28 %), Nickeline (55.15 %), Nickelskutterudite (59.22 %)
AnnabergiteNi3(AsO4)2 · 8H2O59.70%Nickelskutterudite (59.71 %)
SkutteruditeCoAs358.73%Nickelskutterudite (58.74 %)
DolomiteCaMg(CO3)250.48%Nickelskutterudite (50.49 %)
MalachiteCu2(CO3)(OH)240.87%Erythrite (51.09 %)

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])50
37 : Layered igneous intrusions and related PGE minerals43
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]22
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]22
38 : Ophiolites7
36 : Carbonatites, kimberlites, and related igneous rocks7
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)1
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)1
14 : Hot springs, geysers, and other subaerial geothermal minerals0
31 : Thermally altered carbonate, phosphate, and iron formations0