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Predictive Mineralogy

Possible unrecorded species at Ulpen Cu deposit (Ulpen Alp; Kaunz Alp; Hochleger; Keller pass; Öxel valley), Fügenberg, Schwaz District, Tyrol, 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
CalciteCaCO399.99%Ankerite (66.26 %), Annabergite (60.16 %), Baryte (51.88 %), Cobaltite (51.81 %), Dolomite (65.13 %), Erythrite (59.85 %), Glaucodot (58.93 %), Lepidocrocite (55.87 %), Linnaeite (58.18 %), Marcasite (60.67 %), Siderite (52.18 %)
PyrrhotiteFe1-xS82.86%Cobaltite (57.03 %), Glaucodot (60.12 %)
HematiteFe2O355.12%Lepidocrocite (55.13 %)

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: Glaucodot
113
6 : Secondary asteroid phases

Unique: Breunnerite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]33
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]25
37 : Layered igneous intrusions and related PGE minerals15
53 : Other minerals with taphonomic origins8
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]8
50 : Coal and/or oil shale minerals2
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)2
54 : Coal and other mine fire minerals (see also #51 and #56)2
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]2
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)2