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Predictive Mineralogy

Possible unrecorded species at Le Cave (Grasstein), Franzensfeste (Fortezza), Wipptal (Alta Vall'Isarco), South Tyrol, Trentino-Alto Adige (Trentino-South Tyrol), Italy

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
CerussitePbCO392.81%Agardite-(Y) (59.80 %), Mottramite (56.64 %), Wulfenite (58.77 %)
ChalcociteCu2S82.80%Covellite (50.30 %), Digenite (65.40 %)
TitaniteCaTi(SiO4)O77.31%Allanite-(Ce) (52.52 %), Kainosite-(Y) (52.21 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 176.51%Agardite-(Y) (51.96 %), Mottramite (51.11 %)
BorniteCu5FeS468.35%Digenite (68.36 %)
MimetitePb5(AsO4)3Cl53.92%Agardite-(Y) (53.92 %)
CopperCu53.09%Pumpellyite-(Mg) (53.10 %)

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
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Pumpellyite-(Mg)
107
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]23
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]14
34 : Complex granite pegmatites11
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]9
53 : Other minerals with taphonomic origins8
35 : Ultra-alkali and agpaitic igneous rocks7
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)7
26 : Hadean detrital minerals5
19 : Granitic intrusive rocks4
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)3