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Predictive Mineralogy

Possible unrecorded species at La Commanderie mine, Le Temple, Mauléon, Bressuire, Deux-Sèvres, Nouvelle-Aquitaine, 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
ChalcopyriteCuFeS299.89%Bornite (85.52 %), Chalcocite (74.77 %), Marcasite (63.89 %), Metasaléeite (64.29 %), Pyrite (51.72 %), Studtite (53.13 %)
CalciteCaCO381.56%Marcasite (60.67 %), Studtite (53.13 %)
StrengiteFePO4 · 2H2O81.33%Cyrilovite (51.47 %), Natrodufrénite (61.54 %)
MuscoviteKAl2(AlSi3O10)(OH)278.08%Cyrilovite (52.94 %), Leucophosphite (53.44 %)
FluorapatiteCa5(PO4)3F57.35%Cyrilovite (57.35 %)
MalachiteCu2(CO3)(OH)256.19%Chalcocite (56.20 %)
BerauniteFe3+6(PO4)4O(OH)4 · 6H2O53.84%Natrodufrénite (53.85 %)
SphaleriteZnS52.68%Marcasite (65.85 %)
PyrolusiteMn4+O252.33%Cryptomelane (52.34 %)
CovelliteCuS50.00%Metasaléeite (50.00 %)
Rutherfordine(UO2)CO350.00%Studtite (50.00 %)
GalenaPbS46.98%Marcasite (58.73 %)
ArsenopyriteFeAsS40.00%Metasaléeite (50.00 %)

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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]50
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]36
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]33
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)24
21 : Chemically precipitated carbonate, phosphate, iron formations15
31 : Thermally altered carbonate, phosphate, and iron formations14
53 : Other minerals with taphonomic origins14
48 : Soil leaching zone minerals13
34 : Complex granite pegmatites4
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]4