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Predictive Mineralogy

Possible unrecorded species at Ravin de la Craie, Mont-Dore, Issoire, Puy-de-Dôme, 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
QuartzSiO294.23%Alunite (61.80 %), Pyrite (67.27 %), Sulphur (53.86 %)
KaoliniteAl2(Si2O5)(OH)451.68%Alunite (51.69 %)
GypsumCaSO4 · 2H2O50.28%Sulphur (50.28 %)
ChalcopyriteCuFeS241.37%Pyrite (51.72 %)

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
50 : Coal and/or oil shale minerals50
54 : Coal and other mine fire minerals (see also #51 and #56)50
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]47
24 : Authigenic minerals in terrestrial sediments (see also #17)32
49 : Oxic cellular biomineralization (see also #44)29
44 : Anoxic microbially mediated minerals (see also #44)29
47i : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Terrestrial weathering of meteorites]18
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]18
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]18
46 : Near-surface hydrothermal alteration of minerals (see also #22)18