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Predictive Mineralogy

Possible unrecorded species at Vogelhalt mining district, Vogel Alp, Schwarzleograben, Hütten, Leogang, Zell am See District, Salzburg, 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
TyroliteCa2Cu9(AsO4)4(CO3)(OH)8 · 11H2O86.68%Leogangite (68.75 %), Strashimirite (57.39 %)
PyrrhotiteFe1-xS86.43%Mackinawite (71.79 %), Polydymite (51.92 %)
GalenaPbS79.99%Ankerite (54.09 %), Annabergite (57.37 %), Brochantite (55.97 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Devilline (66.36 %), Digenite (59.98 %), Erythrite (53.28 %), Silver (52.62 %), Langite (63.00 %), Lavendulan (54.39 %), Leogangite (68.75 %), Marcasite (58.73 %), Mawsonite (78.07 %), Nickeline (55.15 %), Nickelskutterudite (59.22 %), Olivenite (50.95 %), Polydymite (56.41 %), Posnjakite (59.83 %), Serpierite (74.78 %), Sphalerite (74.68 %), Strashimirite (54.78 %)
CerussitePbCO378.90%Devilline (52.10 %), Langite (53.94 %), Leogangite (56.25 %), Posnjakite (50.00 %), Serpierite (71.59 %)
MagnetiteFe2+Fe3+2O477.60%Mackinawite (54.64 %), Polydymite (50.64 %)
BaryteBaSO477.40%Lavendulan (50.29 %), Leogangite (81.25 %), Strashimirite (65.22 %)
ParnauiteCu9(AsO4)2(SO4)(OH)10 · 7H2O62.50%Leogangite (62.50 %)
SkutteruditeCoAs358.73%Nickelskutterudite (58.74 %)
AdamiteZn2(AsO4)(OH)56.25%Leogangite (56.25 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 155.65%Strashimirite (55.65 %)
StannoiditeCu+6Cu2+2(Fe2+,Zn)3Sn2S1253.50%Mawsonite (53.51 %)
AnglesitePbSO452.40%Serpierite (65.51 %)
LinaritePbCu(SO4)(OH)249.15%Serpierite (61.45 %)
GoldAu44.21%Mawsonite (55.26 %)
MimetitePb5(AsO4)3Cl40.00%Leogangite (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: Mawsonite, Metacinnabar
218
6 : Secondary asteroid phases

Unique: Breunnerite
103
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Polydymite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]74
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]46
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]20
37 : Layered igneous intrusions and related PGE minerals13
56 : Slag and smelter minerals (see also #51 and #55)12
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]11
53 : Other minerals with taphonomic origins8
55 : Anthropogenic mine minerals8
36 : Carbonatites, kimberlites, and related igneous rocks5
38 : Ophiolites5