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Predictive Mineralogy

Possible unrecorded species at Plombières-Vieille Montagne-Moresnet mining district (Plombières-Altenberg-Moresnet mining district), 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
MuscoviteKAl2(AlSi3O10)(OH)298.81%Albite (52.80 %), Goyazite (57.14 %), Kaolinite (51.81 %), Parascholzite (66.67 %), Pyrophyllite (63.67 %)
MimetitePb5(AsO4)3Cl96.50%Beudantite (54.73 %), Ktenasite (52.17 %), Simonkolleite (63.64 %), Zaccagnaite (55.56 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)694.91%Brianyoungite (50.54 %), Fraipontite (56.45 %), Ktenasite (50.00 %), Schulenbergite (52.83 %)
EttringiteCa6Al2(SO4)3(OH)12 · 26H2O87.71%Hydrocalumite (72.97 %), Simonkolleite (54.55 %)
CaledonitePb5Cu2(SO4)3(CO3)(OH)684.26%Elyite (64.52 %), Lanarkite (55.65 %)
BerauniteFe3+6(PO4)4O(OH)4 · 6H2O83.33%Parascholzite (83.33 %)
ArsenopyriteFeAsS75.19%Gersdorffite (50.38 %), Parascholzite (50.00 %)
MicroclineK(AlSi3O8)66.66%Parascholzite (66.67 %)
EosphoriteMn2+Al(PO4)(OH)2 · H2O58.33%Parascholzite (58.33 %)
Heterosite(Fe3+,Mn3+)PO458.33%Parascholzite (58.33 %)
MesseliteCa2Fe2+(PO4)2 · 2H2O58.33%Parascholzite (58.33 %)
RockbridgeiteFe2+Fe3+4(PO4)3(OH)558.33%Parascholzite (58.33 %)
StrunziteMn2+Fe3+2(PO4)2(OH)2 · 6H2O58.33%Parascholzite (58.33 %)
XanthoxeniteCa4Fe3+2(PO4)4(OH)2 · 3H2O58.33%Parascholzite (58.33 %)
FluoriteCaF255.55%Zaccagnaite (55.56 %)
PosnjakiteCu4(SO4)(OH)6 · H2O54.54%Simonkolleite (54.55 %)
AfwilliteCa3(HSiO4)2 · 2H2O54.05%Hydrocalumite (54.05 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 151.61%Fraipontite (51.61 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
Rosasite(Cu,Zn)2(CO3)(OH)250.00%Fraipontite (50.00 %)
AlmandineFe2+3Al2(SiO4)350.00%Parascholzite (50.00 %)
CacoxeniteFe3+24AlO6(PO4)17(OH)12 · 75H2O50.00%Parascholzite (50.00 %)
HureauliteMn2+5(PO3OH)2(PO4)2 · 4H2O50.00%Parascholzite (50.00 %)
LaueiteMn2+Fe3+2(PO4)2(OH)2 · 8H2O50.00%Parascholzite (50.00 %)
MitridatiteCa2Fe3+3(PO4)3O2 · 3H2O50.00%Parascholzite (50.00 %)
PhosphosideriteFePO4 · 2H2O50.00%Parascholzite (50.00 %)
StrengiteFePO4 · 2H2O50.00%Parascholzite (50.00 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O46.66%Parascholzite (58.33 %)
BerylBe3Al2(Si6O18)46.66%Parascholzite (58.33 %)
TriphyliteLiFe2+PO446.66%Parascholzite (58.33 %)
UraniniteUO246.66%Parascholzite (58.33 %)
ZirconZr(SiO4)46.66%Parascholzite (58.33 %)
PerovskiteCaTiO341.08%Hydrocalumite (51.35 %)
SchorlNaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)40.00%Parascholzite (50.00 %)
TorberniteCu(UO2)2(PO4)2 · 12H2O40.00%Parascholzite (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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Fraipontite, Halloysite, Sauconite
388
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
143
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Zaccagnaite
119
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hetaerolite
114
48 : Soil leaching zone minerals

Unique: Gibbsite
103
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)

Unique: Parascholzite
100
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]54
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]41
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])38
55 : Anthropogenic mine minerals35
56 : Slag and smelter minerals (see also #51 and #55)26
37 : Layered igneous intrusions and related PGE minerals25
31 : Thermally altered carbonate, phosphate, and iron formations16
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]15
50 : Coal and/or oil shale minerals14
53 : Other minerals with taphonomic origins13