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Predictive Mineralogy

Possible unrecorded species at Jallet, La Piarre, Gap, Hautes-Alpes, Provence-Alpes-Côte d'Azur, 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
QuartzSiO299.21%Calcite (62.43 %), Cerussite (63.56 %), Galena (65.16 %), Hydrozincite (63.08 %), Smithsonite (55.59 %)
SphaleriteZnS99.09%Cerussite (56.70 %), Galena (65.95 %), Hydrozincite (77.75 %), Smithsonite (72.43 %)
PyriteFeS298.90%Calcite (51.16 %), Cerussite (56.77 %), Galena (66.84 %), Hydrozincite (63.58 %), Smithsonite (57.05 %)
ChalcopyriteCuFeS263.92%Galena (56.79 %), Hydrozincite (53.50 %)
HemimorphiteZn4Si2O7(OH)2 · H2O52.66%Hydrozincite (52.67 %)
MalachiteCu2(CO3)(OH)240.26%Hydrozincite (50.33 %)

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
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
100
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]3
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]3
55 : Anthropogenic mine minerals2
57 : Other minerals formed by human processes2
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)0
14 : Hot springs, geysers, and other subaerial geothermal minerals0
49 : Oxic cellular biomineralization (see also #44)0
31 : Thermally altered carbonate, phosphate, and iron formations0
36 : Carbonatites, kimberlites, and related igneous rocks0
54 : Coal and other mine fire minerals (see also #51 and #56)0