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Predictive Mineralogy

Possible unrecorded species at Pizzo Ragno (Northern slope), Alpe Campra (Campra), Antoliva Valley, Druogno, Verbano-Cusio-Ossola Province, Piedmont, 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
PyriteFeS299.72%Anatase (53.26 %), Hydrokenoelsmoreite (67.80 %), Galena (66.84 %), Galenobismutite (82.95 %), Jarosite (68.24 %)
MuscoviteKAl2(AlSi3O10)(OH)298.93%Bavenite (55.71 %), Bertrandite (60.06 %), Galenobismutite (53.00 %), Tanteuxenite-(Y) (73.68 %), Wagnerite (51.39 %)
AlbiteNa(AlSi3O8)98.13%Allanite-(Ce) (52.28 %), Bavenite (70.59 %), Bertrandite (63.91 %), Tanteuxenite-(Y) (63.16 %)
CalciteCaCO397.99%Bavenite (51.90 %), Galenobismutite (60.37 %), Jarosite (50.12 %), Phlogopite (55.90 %), Titanite (52.17 %)
BerylBe3Al2(Si6O18)82.11%Bavenite (51.21 %), Bertrandite (63.34 %)
ChalcopyriteCuFeS278.47%Hydrokenoelsmoreite (52.54 %), Galena (56.79 %), Galenobismutite (81.11 %), Jarosite (50.73 %)
SphaleriteZnS73.59%Galena (65.95 %), Galenobismutite (76.50 %)
MicroclineK(AlSi3O8)68.42%Tanteuxenite-(Y) (68.42 %)
BismuthiniteBi2S364.05%Galenobismutite (64.06 %)
FerberiteFeWO461.01%Hydrokenoelsmoreite (61.02 %)
PyrrhotiteFe1-xS53.45%Galenobismutite (53.46 %)
FluoriteCaF253.28%Bavenite (53.29 %)
BismuthBi50.69%Galenobismutite (50.69 %)
ArsenopyriteFeAsS44.60%Galenobismutite (55.76 %)
GoldAu43.13%Galenobismutite (53.92 %)
ZirconZr(SiO4)43.09%Allanite-(Ce) (53.87 %)

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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Hydrokenoelsmoreite
100
34 : Complex granite pegmatites21
26 : Hadean detrital minerals17
31 : Thermally altered carbonate, phosphate, and iron formations6
35 : Ultra-alkali and agpaitic igneous rocks4
19 : Granitic intrusive rocks4
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])4
11 : Volcanic fumarole minerals; reduced phases (see also #45)4
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)4
49 : Oxic cellular biomineralization (see also #44)2
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)2