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Predictive Mineralogy
Possible unrecorded species at Val Bona Quarry (Valbona Quarry), Miseglia quarrying basin (Miseglia-Fantiscritti quarrying basin; Fantiscritti quarrying basin), Carrara, Massa-Carrara Province, Tuscany, 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 |
|---|---|---|---|
| Baryte | BaSO4 | 96.02% | Famatinite (51.26 %), Moƫloite (58.33 %), Sulvanite (55.74 %), VƩsigniƩite (55.77 %) |
| Stibnite | Sb2S3 | 92.56% | Moƫloite (75.00 %), Zinkenite (70.26 %) |
| Muscovite | KAl2(AlSi3O10)(OH)2 | 92.46% | Albite (52.80 %), Colusite (52.08 %), Moƫloite (66.67 %) |
| Arsenopyrite | FeAsS | 91.34% | Cannizzarite (52.17 %), Cosalite (55.33 %), Zinkenite (59.48 %) |
| Pyrrhotite | Fe1-xS | 91.29% | Cannizzarite (56.52 %), Cosalite (51.52 %), Smythite (58.70 %) |
| Covellite | CuS | 90.69% | Colusite (54.17 %), Famatinite (51.26 %), Moƫloite (58.33 %) |
| Cerussite | PbCO3 | 84.66% | Moƫloite (66.67 %), Vanadinite (54.01 %) |
| Bornite | Cu5FeS4 | 84.08% | Colusite (61.81 %), Moƫloite (58.33 %) |
| Gypsum | CaSO4 Ā· 2H2O | 83.33% | MoĆ«loite (83.33 %) |
| Jordanite | Pb14As6S23 | 83.33% | Moƫloite (83.33 %) |
| Native Sulphur | S8 | 83.33% | Moƫloite (83.33 %) |
| Bismuthinite | Bi2S3 | 81.90% | Cannizzarite (56.52 %), Cosalite (58.38 %) |
| Azurite | Cu3(CO3)2(OH)2 | 75.00% | Moƫloite (75.00 %) |
| Aragonite | CaCO3 | 66.66% | Moƫloite (66.67 %) |
| Bournonite | PbCuSbS3 | 66.66% | Moƫloite (66.67 %) |
| Celestine | SrSO4 | 66.66% | Moƫloite (83.33 %) |
| Native Gold | Au | 61.47% | Aikinite (52.99 %), Famatinite (50.75 %) |
| Anatase | TiO2 | 58.33% | Moƫloite (58.33 %) |
| Boulangerite | Pb5Sb4S11 | 58.33% | Moƫloite (58.33 %) |
| Digenite | Cu9S5 | 58.33% | Moƫloite (58.33 %) |
| Geocronite | Pb14Sb6S23 | 58.33% | Moƫloite (58.33 %) |
| Luzonite | Cu3AsS4 | 58.33% | Moƫloite (58.33 %) |
| Marcasite | FeS2 | 58.33% | Moƫloite (58.33 %) |
| Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 Ā· nH2O, x < 1 | 53.84% | VĆ©signiĆ©ite (53.85 %) |
| Strontianite | SrCO3 | 53.33% | Moƫloite (66.67 %) |
| Chalcocite | Cu2S | 50.00% | Moƫloite (50.00 %) |
| Dawsonite | NaAlCO3(OH)2 | 50.00% | Moƫloite (50.00 %) |
| Hydrozincite | Zn5(CO3)2(OH)6 | 50.00% | Moƫloite (50.00 %) |
| Semseyite | Pb9Sb8S21 | 50.00% | Moƫloite (50.00 %) |
| Zircon | Zr(SiO4) | 44.01% | Thorite (55.02 %) |
| Wulfenite | Pb(MoO4) | 40.11% | Vanadinite (50.14 %) |
| Kƫsterite | Cu2ZnSnS4 | 40.00% | Moƫloite (50.00 %) |
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.