Predictive Mineralogy
Possible unrecorded species at Alpe Rosso, Orcesco, 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 species | Formula | Match % | Due to recorded presence of |
|---|---|---|---|
| Magnetite | Fe2+Fe3+2O4 | 96.15% | Actinolite (53.38 %), Andradite (57.68 %), Fersmite (56.64 %), Meliphanite (55.10 %) |
| Chalcopyrite | CuFeS2 | 79.53% | Actinolite (52.26 %), Anglesite (58.14 %), Arsenopyrite (61.33 %), Galena (56.79 %), Malayaite (64.29 %), Pyrite (51.72 %) |
| Sphalerite | ZnS | 79.27% | Anglesite (64.09 %), Arsenopyrite (55.02 %), Cerussite (56.70 %), Galena (65.95 %), Malayaite (61.90 %) |
| Diopside | CaMgSi2O6 | 78.40% | Grossular (52.27 %), Malayaite (54.76 %) |
| Natrolite | Na2Al2Si3O10 · 2H2O | 67.34% | Meliphanite (67.35 %) |
| Pyrrhotite | Fe1-xS | 64.28% | Malayaite (64.29 %) |
| Nepheline | Na3K(Al4Si4O16) | 63.26% | Meliphanite (63.27 %) |
| Uraninite | UO2 | 61.27% | Uranophane (61.27 %) |
| Aegirine | NaFe3+Si2O6 | 59.18% | Meliphanite (59.18 %) |
| Molybdenite | MoS2 | 58.77% | Meliphanite (73.47 %) |
| Chromite | Fe2+Cr3+2O4 | 57.93% | Uvarovite (57.94 %) |
| Spodumene | LiAlSi2O6 | 54.54% | Bityite (54.55 %) |
| Columbite-(Fe) | Fe2+Nb2O6 | 54.05% | Tantalite-(Fe) (54.05 %) |
| Corundum | Al2O3 | 53.47% | Margarite (53.48 %) |
| Spessartine | Mn2+3Al2(SiO4)3 | 51.51% | Bityite (51.52 %) |
| Helvine | Be3Mn2+4(SiO4)3S | 51.02% | Meliphanite (51.02 %) |
| Ilmenite | Fe2+TiO3 | 50.00% | Vigezzite (50.00 %) |
| Monazite-(Ce) | Ce(PO4) | 50.00% | Hydroxycalciomicrolite (50.00 %) |
| Scheelite | Ca(WO4) | 43.80% | Malayaite (54.76 %) |
| Copper | Cu | 42.47% | Pumpellyite-(Mg) (53.10 %) |
| Malachite | Cu2(CO3)(OH)2 | 40.27% | Anglesite (50.35 %) |
| Wulfenite | Pb(MoO4) | 40.11% | Vanadinite (50.14 %) |
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.