Predictive Mineralogy
Possible unrecorded species at Bec di Nona (Becca di Nona; Bec-de-Nona; Lac de Leser - Bec-de-Nona area), Champdepraz, Aosta Valley, 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 |
---|---|---|---|
Quartz | SiO2 | 99.99% | Allanite-(Ce) (73.19 %), Clinochlore (65.82 %), Clinozoisite (72.76 %), Diopside (51.68 %), Epidote (69.84 %), Fluorapatite (70.90 %), Grossular (59.42 %), Ilmenite (52.06 %), Magnetite (50.54 %), Titanite (65.16 %), Vesuvianite (53.96 %) |
Calcite | CaCO3 | 99.85% | Clinochlore (54.46 %), Clinozoisite (56.64 %), Diopside (54.07 %), Epidote (51.60 %), Grossular (59.86 %), Perovskite (58.08 %), Titanite (52.17 %), Vesuvianite (57.54 %) |
Pyrite | FeS2 | 89.84% | Clinochlore (51.79 %), Clinozoisite (51.74 %), Epidote (56.37 %) |
Albite | Na(AlSi3O8) | 52.27% | Allanite-(Ce) (52.28 %) |
Zircon | Zr(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.