Predictive Mineralogy
Possible unrecorded species at Val Gardena Sandstone exposure near San Lugano pass, Carano, Ville di Fiemme, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), 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 |
---|---|---|---|
Arsenopyrite | FeAsS | 94.79% | Arthurite (51.28 %), Pharmacosiderite (58.74 %), Scorodite (74.10 %) |
Jarosite | KFe3+3(SO4)2(OH)6 | 91.79% | Arthurite (58.97 %), Middlebackite (80.00 %) |
Smithsonite | ZnCO3 | 78.95% | Aurichalcite (54.58 %), Zincolivenite (53.66 %) |
Mimetite | Pb5(AsO4)3Cl | 77.06% | Arthurite (51.28 %), Beudantite (54.73 %), Parnauite (51.20 %), Zincolivenite (65.85 %) |
Copper | Cu | 75.83% | Arthurite (51.28 %), Parnauite (50.40 %) |
Hematite | Fe2O3 | 54.45% | Zálesíite (54.46 %) |
Hemimorphite | Zn4Si2O7(OH)2 · H2O | 50.46% | Aurichalcite (50.47 %) |
Adamite | Zn2(AsO4)(OH) | 50.00% | Zincolivenite (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.