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Predictive Mineralogy

Possible unrecorded species at Ravinella di Sotto Mine, Forno, Valstrona, 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
CalciteCaCO399.99%Axinite-(Fe) (53.22 %), Axinite-(Mn) (56.60 %), Bustamite (65.55 %), Clinozoisite (56.64 %), Hedenbergite (60.34 %), Johannsenite (74.19 %), Manganilvaite (87.50 %), Prehnite (61.24 %), Pyroxmangite (53.01 %), Wollastonite (65.90 %)
PyriteFeS299.98%Bustamite (58.82 %), Chalcopyrite (75.16 %), Clinozoisite (51.74 %), Hedenbergite (52.35 %), Johannsenite (66.67 %), Manganilvaite (62.50 %), Pyroxmangite (52.41 %), Pyrrhotite (80.12 %), Wollastonite (51.22 %)
Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)89.84%Axinite-(Fe) (50.85 %), Clinozoisite (56.31 %), Johannsenite (52.69 %)
SphaleriteZnS79.69%Bustamite (53.78 %), Chalcopyrite (50.66 %), Johannsenite (69.89 %), Manganilvaite (87.50 %), Pyrrhotite (55.40 %)
MuscoviteKAl2(AlSi3O10)(OH)278.52%Albite (52.80 %), Spessartine (54.51 %)
GalenaPbS78.47%Chalcopyrite (51.07 %), Johannsenite (68.82 %), Manganilvaite (87.50 %)
RhodochrositeMnCO374.69%Pyroxmangite (74.70 %)
MagnetiteFe2+Fe3+2O457.46%Hedenbergite (57.46 %)
TephroiteMn2+2SiO454.81%Pyroxmangite (54.82 %)
DiopsideCaMgSi2O650.54%Wollastonite (50.54 %)

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
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Johannsenite
123
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Manganilvaite
100
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])12
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)10
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)7
34 : Complex granite pegmatites6
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]5
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]4
20 : Acidic volcanic rocks4
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)2
56 : Slag and smelter minerals (see also #51 and #55)1
24 : Authigenic minerals in terrestrial sediments (see also #17)1