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Predictive Mineralogy

Possible unrecorded species at H眉ttenberger Erzberg, H眉ttenberg, Sankt Veit an der Glan 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
ZeuneriteCu(UO2)2(AsO4)2 路 12H2O84.31%Kahlerite (52.94 %), Metakahlerite (66.67 %)
CupriteCu2O82.24%Delafossite (82.25 %)
AutuniteCa(UO2)2(PO4)2 路 10-12H2O78.31%Sal茅eite (55.45 %), Uranopilite (51.33 %)
CopperCu67.45%Delafossite (67.46 %)
MetazeuneriteCu(UO2)2(AsO4)2 路 8H2O66.66%Metakahlerite (66.67 %)
CassiteriteSnO261.83%Stannite (61.84 %)
Schoepite(UO2)8O2(OH)12 路 12H2O58.82%Kahlerite (58.82 %)
CubaniteCuFe2S356.27%Valleriite (56.27 %)
TephroiteMn2+2SiO454.81%Pyroxmangite (54.82 %)
Meta-autuniteCa(UO2)2(PO4)2 路 6H2O52.94%Kahlerite (52.94 %)
TorberniteCu(UO2)2(PO4)2 路 12H2O52.21%Uranopilite (52.21 %)

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: Argentopyrite, Arsenic, Boulangerite, Bournonite, Matildite, Pararammelsbergite, etc.
1,242
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Metakahlerite
201
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite
147
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Kutnohorite
101
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]100
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Famatinite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)62
34 : Complex granite pegmatites33
26 : Hadean detrital minerals28
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]28
37 : Layered igneous intrusions and related PGE minerals27
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)24
53 : Other minerals with taphonomic origins21
13 : Hadean serpentinization17
36 : Carbonatites, kimberlites, and related igneous rocks16