Predictive Mineralogy
Possible unrecorded species at Fianel, Ausserferrera, Ferrera, Viamala Region, Grisons, Switzerland
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 |
---|---|---|---|
Pyrite | FeS2 | 100.00% | Allanite-(La) (55.17 %), Baryte (50.79 %), Dolomite (58.22 %), Goldmanite (75.00 %), Hematite (50.17 %), Kutnohorite (63.08 %), LĂ„ngbanite (50.00 %), OxycalcioromeÌite (100.00 %), RanciĂ©ite (53.37 %), Siderite (66.11 %) |
Calcite | CaCO3 | 100.00% | Allanite-(La) (58.62 %), Ansermetite (70.00 %), Barylite (71.43 %), Baryte (51.88 %), Bergslagite (77.78 %), Calderite (59.09 %), Dolomite (65.13 %), FluorcalcioromĂ©ite (53.33 %), Goldmanite (66.67 %), Hausmannite (51.00 %), Jacobsite (52.02 %), Kutnohorite (81.00 %), LĂ„ngbanite (80.00 %), Manganberzeliite (79.31 %), Medaite (83.33 %), Nambulite (50.00 %), OxycalcioromeÌite (100.00 %), Palenzonaite (80.00 %), Parsettensite (76.09 %), Pyrobelonite (89.66 %), RanciĂ©ite (73.56 %), Saneroite (83.33 %), Siderite (52.18 %), Tiragalloite (77.78 %), Wallkilldellite (77.27 %) |
Malachite | Cu2(CO3)(OH)2 | 100.00% | Medaite (83.33 %), OxycalcioromeÌite (100.00 %), Palenzonaite (60.00 %), Saneroite (83.33 %), Tiragalloite (50.00 %), Volborthite (64.20 %), Wallkilldellite (54.55 %) |
Rhodochrosite | MnCO3 | 99.99% | Calderite (59.09 %), Fluorcalcioroméite (53.33 %), Hausmannite (51.25 %), Jacobsite (61.62 %), Kutnohorite (69.18 %), LÄngbanite (60.00 %), Manganberzeliite (65.52 %), Medaite (83.33 %), Nambulite (68.75 %), Palenzonaite (80.00 %), Parsettensite (71.74 %), Pyrobelonite (68.97 %), Saneroite (83.33 %), Tiragalloite (88.89 %), Wallkilldellite (50.00 %) |
Albite | Na(AlSi3O8) | 99.99% | Allanite-(La) (58.62 %), Barylite (66.67 %), Bergslagite (55.56 %), Chernovite-(Y) (52.63 %), FluorcalcioromĂ©ite (53.33 %), LĂ„ngbanite (60.00 %), Manganberzeliite (58.62 %), Medaite (66.67 %), Monazite-(Ce) (51.78 %), OxycalcioromeÌite (80.00 %), Palenzonaite (60.00 %), Parsettensite (50.00 %), Phenakite (59.33 %), Pyrobelonite (51.72 %), Saneroite (66.67 %), Tiragalloite (66.67 %), Wallkilldellite (54.55 %) |
Chalcopyrite | CuFeS2 | 99.88% | Goldmanite (52.78 %), Medaite (83.33 %), OxycalcioromeÌite (80.00 %), Saneroite (66.67 %), Siderite (51.43 %), Wallkilldellite (54.55 %) |
Spessartine | Mn2+3Al2(SiO4)3 | 99.84% | Bergslagite (55.56 %), Calderite (72.73 %), Fluorcalcioroméite (53.33 %), LÄngbanite (70.00 %), Manganberzeliite (58.62 %), Nambulite (56.25 %), Tiragalloite (50.00 %) |
Pyrophanite | Mn2+TiO3 | 99.44% | LĂ„ngbanite (60.00 %), Medaite (66.67 %), Nambulite (50.00 %), Palenzonaite (70.00 %), Tiragalloite (72.22 %) |
Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) | 99.30% | LĂ„ngbanite (60.00 %), Medaite (66.67 %), Palenzonaite (60.00 %), Saneroite (66.67 %), Tiragalloite (61.11 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 99.25% | Bergslagite (66.67 %), Beryl (55.56 %), Chernovite-(Y) (56.14 %), Goldmanite (52.78 %), Monazite-(Ce) (51.26 %), Tiragalloite (50.00 %) |
Neotocite | (Mn,Fe,Mg)SiO3 · H2O | 99.16% | Medaite (66.67 %), Palenzonaite (70.00 %), Saneroite (83.33 %), Tiragalloite (50.00 %) |
Tephroite | Mn2+2SiO4 | 98.87% | LĂ„ngbanite (50.00 %), Manganberzeliite (55.17 %), Nambulite (62.50 %), Palenzonaite (60.00 %), Tiragalloite (66.67 %) |
Chalcocite | Cu2S | 97.77% | Medaite (66.67 %), OxycalcioromeÌite (80.00 %), Saneroite (66.67 %) |
Gypsum | CaSO4 · 2H2O | 97.77% | Ansermetite (60.00 %), Medaite (66.67 %), Saneroite (83.33 %) |
Sarkinite | Mn2+2(AsO4)(OH) | 97.22% | LĂ„ngbanite (50.00 %), Medaite (66.67 %), Saneroite (66.67 %), Tiragalloite (50.00 %) |
Copper | Cu | 97.22% | Medaite (83.33 %), Palenzonaite (50.00 %), Saneroite (66.67 %) |
Fluorite | CaF2 | 96.97% | Barylite (61.90 %), Bergslagite (66.67 %), LĂ„ngbanite (50.00 %), Phenakite (52.33 %) |
Pyroxmangite | Mn2+SiO3 | 95.83% | Calderite (50.00 %), Medaite (66.67 %), Palenzonaite (50.00 %), Tiragalloite (50.00 %) |
Magnetite | Fe2+Fe3+2O4 | 95.78% | Allanite-(La) (55.17 %), Calderite (54.55 %), LĂ„ngbanite (50.00 %), Pyrobelonite (58.62 %) |
Caryopilite | Mn2+3Si2O5(OH)4 | 94.92% | Medaite (66.67 %), Parsettensite (54.35 %), Saneroite (66.67 %) |
Ganophyllite | (K,Na,Ca)2Mn8(Si,Al)12(O,OH)32 · 8H2O | 94.44% | Medaite (66.67 %), Saneroite (83.33 %) |
Titanite | CaTi(SiO4)O | 93.10% | Allanite-(La) (58.62 %), Palenzonaite (50.00 %), Saneroite (66.67 %) |
Azurite | Cu3(CO3)2(OH)2 | 90.00% | OxycalcioromeÌite (80.00 %), Wallkilldellite (50.00 %) |
Cuprite | Cu2O | 88.88% | Medaite (66.67 %), Saneroite (66.67 %) |
Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) | 88.88% | Medaite (66.67 %), Saneroite (66.67 %) |
Opal | SiO2 · nH2O | 83.33% | Palenzonaite (50.00 %), Saneroite (66.67 %) |
Stibnite | Sb2S3 | 80.00% | OxycalcioromeÌite (80.00 %) |
Rutile | TiO2 | 78.94% | Bergslagite (55.56 %), Chernovite-(Y) (52.63 %) |
Axinite-(Mn) | Ca2Mn2+Al2BSi4O15(OH) | 77.77% | Medaite (83.33 %), Palenzonaite (50.00 %), Saneroite (66.67 %) |
Zircon | Zr(SiO4) | 77.12% | Allanite-(La) (62.07 %), Barylite (57.14 %), Chernovite-(Y) (50.88 %), Monazite-(Ce) (54.99 %) |
Goethite | α-Fe3+O(OH) | 75.00% | Ranciéite (50.00 %), Wallkilldellite (50.00 %) |
Microcline | K(AlSi3O8) | 71.42% | Barylite (71.43 %) |
Gamagarite | Ba2Fe3+(VO4)2(OH) | 66.66% | Saneroite (66.67 %) |
Pyrolusite | Mn4+O2 | 63.98% | Manganite (63.98 %) |
Sphalerite | ZnS | 60.95% | Barylite (52.38 %), LĂ„ngbanite (50.00 %) |
Pascoite | Ca2Ca(V10O28) · 17H2O | 60.00% | Ansermetite (60.00 %) |
Molybdenite | MoS2 | 55.99% | Powellite (55.99 %) |
Aragonite | CaCO3 | 55.55% | Bergslagite (55.56 %) |
Tilasite | CaMg(AsO4)F | 55.55% | Bergslagite (55.56 %) |
Xenotime-(Y) | Y(PO4) | 54.38% | Chernovite-(Y) (54.39 %) |
Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) | 51.72% | Allanite-(La) (51.72 %) |
Pyrrhotite | Fe1-xS | 50.00% | Goldmanite (50.00 %) |
Carnotite | K2(UO2)2(VO4)2 · 3H2O | 40.00% | Ansermetite (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.