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Predictive Mineralogy

Possible unrecorded species at Umberg, Wernberg, Villach-Land District, Carinthia, Austria

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
CerussitePbCO385.48%Hydrozincite (67.25 %), Smithsonite (55.69 %)
ArsenopyriteFeAsS75.45%Boulangerite (64.45 %), Bournonite (55.79 %), Jamesonite (63.81 %)
MuscoviteKAl2(AlSi3O10)(OH)256.04%Almandine (56.05 %)
HemimorphiteZn4Si2O7(OH)2 · H2O52.66%Hydrozincite (52.67 %)
GypsumCaSO4 · 2H2O50.28%Sulphur (50.28 %)

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: Boulangerite, Bournonite, Freibergite Subgroup
299
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]15
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)14
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]13
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]4
53 : Other minerals with taphonomic origins4
55 : Anthropogenic mine minerals3
50 : Coal and/or oil shale minerals3
54 : Coal and other mine fire minerals (see also #51 and #56)3
26 : Hadean detrital minerals2
36 : Carbonatites, kimberlites, and related igneous rocks2