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Predictive Mineralogy

Possible unrecorded species at Tempel, Scoufour (Bonnac North), Bonnac, Saint-Flour, 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
PyriteFeS299.99%Arsenopyrite (79.40 %), Bismuth (65.41 %), Bismuthinite (76.49 %), Calcite (51.16 %), Chalcopyrite (75.16 %), Ferberite (59.80 %), Löllingite (66.48 %), Marcasite (86.56 %), Molybdenite (68.29 %), Pyrrhotite (80.12 %), Siderite (66.11 %), Sphalerite (75.10 %), Tetradymite (77.65 %)
GalenaPbS79.92%Arsenopyrite (53.61 %), Bismuth (51.78 %), Bismuthinite (57.89 %), Chalcopyrite (51.07 %), Löllingite (53.52 %), Marcasite (58.73 %), Sphalerite (74.68 %), Tetradymite (60.52 %)

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
34 : Complex granite pegmatites50
31 : Thermally altered carbonate, phosphate, and iron formations35
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])30
26 : Hadean detrital minerals24
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)15
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)11
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]11
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]11
50 : Coal and/or oil shale minerals10
54 : Coal and other mine fire minerals (see also #51 and #56)10