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Predictive Mineralogy

Possible unrecorded species at Burgum Alp, Pfitsch (Val di Vizze), 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
MuscoviteKAl2(AlSi3O10)(OH)298.51%Albite (52.80 %), Euclase (69.57 %), Margarite (54.55 %), Monazite-(Ce) (51.26 %), Xenotime-(Y) (53.30 %)
GalenaPbS62.02%Ankerite (54.09 %), Chalcopyrite (51.07 %)
SphaleriteZnS61.59%Ankerite (53.36 %), Chalcopyrite (50.66 %)
BerylBe3Al2(Si6O18)55.79%Euclase (55.80 %)
CorundumAl2O353.47%Margarite (53.48 %)

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
6 : Secondary asteroid phases

Unique: Breunnerite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)24
34 : Complex granite pegmatites16
31 : Thermally altered carbonate, phosphate, and iron formations14
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]12
26 : Hadean detrital minerals8
38 : Ophiolites6
35 : Ultra-alkali and agpaitic igneous rocks5
13 : Hadean serpentinization5
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)5
36 : Carbonatites, kimberlites, and related igneous rocks2