Predictive Mineralogy
Possible unrecorded species at Pizzo Marcio South-East dyke, 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 species | Formula | Match % | Due to recorded presence of |
|---|---|---|---|
| Magnetite | Fe2+Fe3+2O4 | 79.78% | Actinolite (53.38 %), Fersmite (56.64 %) |
| Chalcopyrite | CuFeS2 | 72.03% | Actinolite (52.26 %), Galena (56.79 %), Pyrite (51.72 %) |
| Analcime | Na(AlSi2O6) · H2O | 57.41% | Thomsonite-Ca (57.41 %) |
| Cerussite | PbCO3 | 54.00% | Vanadinite (54.01 %) |
| Corundum | Al2O3 | 53.47% | Margarite (53.48 %) |
| Fluorapatite | Ca5(PO4)3F | 53.09% | Fersmite (53.10 %) |
| Sphalerite | ZnS | 52.75% | Galena (65.95 %) |
| Copper | Cu | 42.47% | Pumpellyite-(Mg) (53.10 %) |
| 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.