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Predictive Mineralogy

Possible unrecorded species at Mine Jaune, Grandfontaine, Molsheim, Bas-Rhin, Grand Est, 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)297.93%Azurite (89.71 %), Chalcocite (56.20 %), Digenite (54.15 %)
MuscoviteKAl2(AlSi3O10)(OH)295.87%Albite (52.80 %), Bertrandite (60.06 %), Beryl (55.56 %), Topaz (50.72 %)
CovelliteCuS71.99%Digenite (72.00 %)
BorniteCu5FeS468.35%Digenite (68.36 %)
GypsumCaSO4 · 2H2O64.75%Fibroferrite (64.75 %)
MelanteriteFe2+(H2O)6SO4 · H2O54.91%Fibroferrite (54.92 %)
KaoliniteAl2(Si2O5)(OH)451.68%Alunite (51.69 %)

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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])31
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)30
6 : Secondary asteroid phases28
31 : Thermally altered carbonate, phosphate, and iron formations14
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]12
26 : Hadean detrital minerals11
19 : Granitic intrusive rocks10
35 : Ultra-alkali and agpaitic igneous rocks10
53 : Other minerals with taphonomic origins9