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Predictive Mineralogy

Possible unrecorded species at Bancarel, Leucamp, Aurillac, Cantal, Auvergne-Rhône-Alpes, 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
MalachiteCu2(CO3)(OH)280.13%Chalcocite (56.20 %), Covellite (54.66 %)
GalenaPbS79.99%Arsenopyrite (53.61 %), Bismuth (51.78 %), Bismuthinite (57.89 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Cubanite (63.07 %), Marcasite (58.73 %), Pharmacosiderite (51.63 %), Scorodite (50.30 %), Sphalerite (74.68 %), Tetradymite (60.52 %)
MuscoviteKAl2(AlSi3O10)(OH)262.63%Schorl (62.64 %)
CalciteCaCO360.67%Marcasite (60.67 %)
MagnetiteFe2+Fe3+2O457.23%Cubanite (57.24 %)

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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]41
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]41
6 : Secondary asteroid phases33
31 : Thermally altered carbonate, phosphate, and iron formations28
34 : Complex granite pegmatites25
26 : Hadean detrital minerals21
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)12
55 : Anthropogenic mine minerals10
54 : Coal and other mine fire minerals (see also #51 and #56)8