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Predictive Mineralogy

Possible unrecorded species at Liauzun, Olloix, Clermont-Ferrand, 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
GalenaPbS99.99%Anglesite (86.19 %), Bariopharmacosiderite (53.23 %), Beudantite (76.34 %), Cerussite (83.05 %), Chalcopyrite (51.07 %), Clausthalite (61.11 %), Covellite (64.18 %), Digenite (59.98 %), Marcasite (58.73 %), Mimetite (75.78 %)
CalciteCaCO399.99%Anglesite (53.86 %), Bariopharmacosiderite (52.15 %), Baryte (51.88 %), Cerussite (50.77 %), Clausthalite (58.61 %), Digenite (52.28 %), Jarosite (50.12 %), Marcasite (60.67 %), Mimetite (56.29 %), Olsacherite (80.00 %), Penroseite (62.50 %), Selenium (51.83 %)
MalachiteCu2(CO3)(OH)299.98%Anglesite (50.35 %), Bariopharmacosiderite (65.05 %), Beudantite (59.67 %), Chalcocite (56.20 %), Chalcomenite (58.33 %), Covellite (54.66 %), Digenite (54.15 %), Mimetite (60.02 %), Olsacherite (73.33 %), Zeunerite (51.16 %)
HematiteFe2O396.00%Chalcomenite (52.08 %), Olsacherite (73.33 %), Penroseite (68.75 %)
Goethiteα-Fe3+O(OH)94.93%Bariopharmacosiderite (52.69 %), Beudantite (54.12 %), Olsacherite (53.33 %), Penroseite (50.00 %)
SphaleriteZnS79.97%Anglesite (64.09 %), Beudantite (60.29 %), Cerussite (56.70 %), Chalcopyrite (50.66 %), Clausthalite (53.06 %), Covellite (64.68 %), Digenite (61.34 %), Marcasite (65.85 %), Mimetite (53.11 %)
BorniteCu5FeS468.35%Digenite (68.36 %)
GoldAu62.88%Clausthalite (51.11 %), Penroseite (56.25 %)
AzuriteCu3(CO3)2(OH)254.30%Bariopharmacosiderite (54.30 %)
BrochantiteCu4(SO4)(OH)651.61%Bariopharmacosiderite (51.61 %)
OliveniteCu2(AsO4)(OH)51.07%Bariopharmacosiderite (51.08 %)
DolomiteCaMg(CO3)250.00%Penroseite (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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Clausthalite, Penroseite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]30
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]23
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]16
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]5
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]4
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]4
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]3
50 : Coal and/or oil shale minerals2
54 : Coal and other mine fire minerals (see also #51 and #56)2
27 : Radioactive decay; auto-oxidation2