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Predictive Mineralogy

Possible unrecorded species at Thier del Preu quarry, Petit-Sart, Lierneux, Liège, Wallonia, Belgium

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
PyriteFeS295.08%Anatase (53.26 %), Hematite (50.17 %), Muscovite (50.01 %), Pyrophyllite (57.79 %)
Piemontite(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)65.00%Ardennite-(As) (65.00 %)
CalciteCaCO352.50%Ardennite-(As) (52.50 %)
PyrolusiteMn4+O252.33%Cryptomelane (52.34 %)
AlbiteNa(AlSi3O8)50.00%Ardennite-(As) (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
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Ardennite-(As)
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]16
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]12
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)8
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]7
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]7
48 : Soil leaching zone minerals5
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)4
24 : Authigenic minerals in terrestrial sediments (see also #17)4
34 : Complex granite pegmatites3
21 : Chemically precipitated carbonate, phosphate, iron formations1