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Predictive Mineralogy

Possible unrecorded species at Pizzo Marcio, Trontano, 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
FluorapatiteCa5(PO4)3F91.06%Ferrowodginite (61.90 %), Fersmite (53.10 %), Vigezzite (50.00 %)
MagnetiteFe2+Fe3+2O490.92%Actinolite (53.38 %), Fersmite (56.64 %), Meliphanite (55.10 %)
ChalcopyriteCuFeS278.69%Actinolite (52.26 %), Anglesite (58.14 %), Galena (56.79 %), Molybdenite (60.83 %), Pyrite (51.72 %)
SphaleriteZnS75.76%Anglesite (64.09 %), Cerussite (56.70 %), Galena (65.95 %)
NatroliteNa2Al2Si3O10 · 2H2O67.34%Meliphanite (67.35 %)
NephelineNa3K(Al4Si4O16)63.26%Meliphanite (63.27 %)
UraniniteUO261.27%Uranophane (61.27 %)
AegirineNaFe3+Si2O659.18%Meliphanite (59.18 %)
CorundumAl2O353.47%Margarite (53.48 %)
HelvineBe3Mn2+4(SiO4)3S51.02%Meliphanite (51.02 %)
WulfenitePb(MoO4)50.13%Vanadinite (50.14 %)
IlmeniteFe2+TiO350.00%Vigezzite (50.00 %)
CopperCu42.47%Pumpellyite-(Mg) (53.10 %)
MalachiteCu2(CO3)(OH)240.27%Anglesite (50.35 %)

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
34 : Complex granite pegmatites

Unique: Ferrowodginite, Hydroxycalciomicrolite, Microlite Group, Oxycalciomicrolite, Tantalite-(Mn), Tapiolite-(Fe)
570
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)

Unique: Gismondine Subgroup, Roggianite
166
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Pumpellyite-(Mg)
103
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Meliphanite
100
26 : Hadean detrital minerals43
36 : Carbonatites, kimberlites, and related igneous rocks32
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)21
31 : Thermally altered carbonate, phosphate, and iron formations17
19 : Granitic intrusive rocks10
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]9
6 : Secondary asteroid phases7
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)4
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]3
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]3