Predictive Mineralogy
Possible unrecorded species at Ênio claim, Laranjeiras, Galiléia, Minas Gerais, Brazil
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 | 100.00% | Alluaudite (77.36 %), Amblygonite (78.62 %), Arrojadite-(KFe) (80.00 %), Arsenopyrite (80.07 %), Beryllonite (90.00 %), Bismuth (78.36 %), Bornite (66.21 %), Chalcopyrite (67.26 %), Childrenite (87.04 %), Claudetite (75.00 %), Columbite-(Fe) (79.59 %), Covellite (76.39 %), Cubanite (63.93 %), Cyrilovite (79.41 %), Ferberite (76.94 %), Fluorapatite (70.90 %), Galena (65.16 %), Goethite (66.86 %), Graftonite (71.31 %), Greifensteinite (93.55 %), Heterosite (71.04 %), Hydroxylherderite (90.15 %), Laueite (82.28 %), Löllingite (76.36 %), Ludlamite (86.67 %), Messelite (77.55 %), Montebrasite (91.88 %), Phosphoferrite (91.18 %), Phosphosiderite (78.20 %), Phosphuranylite (60.00 %), Pyrite (67.27 %), Pyrrhotite (67.51 %), Rockbridgeite (71.49 %), Roscherite (88.46 %), Saléeite (56.36 %), Sarcopside (60.56 %), Sphalerite (67.53 %), Sulphur (53.86 %), Tavorite (87.18 %), Triphylite (78.03 %), Uraninite (52.94 %), Vivianite (55.13 %), Whiteite-(CaFeMg) (77.78 %), Wolfeite (74.51 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 99.99% | Alluaudite (74.53 %), Amblygonite (69.57 %), Arrojadite-(KFe) (60.00 %), Beryllonite (80.00 %), Childrenite (61.11 %), Columbite-(Fe) (70.50 %), Cyrilovite (52.94 %), Graftonite (73.77 %), Greifensteinite (80.65 %), Heterosite (67.87 %), Hydroxylherderite (84.09 %), Laueite (78.48 %), Ludlamite (76.00 %), Messelite (69.39 %), Montebrasite (86.32 %), Phosphoferrite (79.41 %), Phosphosiderite (56.87 %), Rockbridgeite (56.14 %), Roscherite (76.92 %), Sarcopside (66.20 %), Tavorite (84.62 %), Triphylite (76.88 %), Wolfeite (76.47 %) |
Albite | Na(AlSi3O8) | 99.99% | Alluaudite (66.98 %), Amblygonite (69.20 %), Arrojadite-(KFe) (53.33 %), Beryllonite (84.00 %), Childrenite (50.93 %), Columbite-(Fe) (66.38 %), Graftonite (57.38 %), Greifensteinite (83.87 %), Heterosite (65.16 %), Hydroxylherderite (87.88 %), Laueite (77.22 %), Ludlamite (57.33 %), Messelite (63.27 %), Montebrasite (81.62 %), Phosphoferrite (76.47 %), Roscherite (69.23 %), Tavorite (76.92 %), Triphylite (68.79 %), Wolfeite (54.90 %) |
Beryl | Be3Al2(Si6O18) | 99.99% | Alluaudite (66.04 %), Amblygonite (65.22 %), Arrojadite-(KFe) (61.67 %), Beryllonite (78.00 %), Columbite-(Fe) (57.46 %), Graftonite (55.74 %), Greifensteinite (77.42 %), Heterosite (66.52 %), Hydroxylherderite (87.12 %), Laueite (74.68 %), Ludlamite (50.67 %), Messelite (57.14 %), Montebrasite (71.37 %), Phosphoferrite (61.76 %), Roscherite (65.38 %), Tavorite (71.79 %), Triphylite (71.97 %), Wolfeite (56.86 %) |
Microcline | K(AlSi3O8) | 99.99% | Alluaudite (57.55 %), Beryllonite (72.00 %), Columbite-(Fe) (55.92 %), Greifensteinite (74.19 %), Heterosite (56.56 %), Hydroxylherderite (77.27 %), Laueite (73.42 %), Messelite (57.14 %), Montebrasite (62.82 %), Phosphoferrite (58.82 %), Roscherite (61.54 %), Tavorite (76.92 %), Triphylite (55.49 %) |
Siderite | FeCO3 | 98.80% | Laueite (50.63 %), Ludlamite (65.33 %), Messelite (59.18 %), Roscherite (61.54 %), Whiteite-(CaFeMg) (55.56 %) |
Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | 98.64% | Greifensteinite (58.06 %), Laueite (51.90 %), Phosphuranylite (64.29 %), Roscherite (57.69 %), Saléeite (55.45 %) |
Hureaulite | Mn2+5(PO3OH)2(PO4)2 · 4H2O | 98.24% | Laueite (54.43 %), Phosphoferrite (50.00 %), Tavorite (92.31 %) |
Beraunite | Fe3+6(PO4)4O(OH)4 · 6H2O | 98.23% | Laueite (64.56 %), Messelite (53.06 %), Phosphoferrite (52.94 %), Rockbridgeite (54.82 %), Roscherite (50.00 %) |
Strengite | FePO4 · 2H2O | 97.87% | Cyrilovite (51.47 %), Laueite (50.63 %), Phosphosiderite (53.55 %), Rockbridgeite (50.44 %), Tavorite (61.54 %) |
Mitridatite | Ca2Fe3+3(PO4)3O2 · 3H2O | 93.76% | Laueite (64.56 %), Messelite (51.02 %), Tavorite (64.10 %) |
Eosphorite | Mn2+Al(PO4)(OH)2 · H2O | 92.79% | Beryllonite (52.00 %), Greifensteinite (64.52 %), Roscherite (57.69 %) |
Strunzite | Mn2+Fe3+2(PO4)2(OH)2 · 6H2O | 82.23% | Greifensteinite (51.61 %), Laueite (63.29 %) |
Gypsum | CaSO4 · 2H2O | 80.11% | Claudetite (60.00 %), Sulphur (50.28 %) |
Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 79.99% | Alluaudite (51.89 %), Beryllonite (60.00 %), Graftonite (50.82 %), Greifensteinite (70.97 %), Hydroxylherderite (69.70 %), Laueite (56.96 %), Messelite (55.10 %), Montebrasite (54.27 %), Phosphoferrite (58.82 %), Roscherite (50.00 %), Tavorite (51.28 %), Triphylite (52.60 %), Wolfeite (62.75 %) |
Calcite | CaCO3 | 77.96% | Claudetite (55.00 %), Löllingite (51.02 %) |
Zircon | Zr(SiO4) | 77.27% | Columbite-(Fe) (56.78 %), Greifensteinite (61.29 %), Laueite (51.90 %), Roscherite (57.69 %) |
Cassiterite | SnO2 | 76.78% | Greifensteinite (54.84 %), Hydroxylherderite (51.52 %), Montebrasite (63.25 %), Roscherite (50.00 %) |
Leucophosphite | KFe3+2(PO4)2(OH) · 2H2O | 61.53% | Tavorite (61.54 %) |
Spodumene | LiAlSi2O6 | 58.54% | Montebrasite (58.55 %) |
Magnetite | Fe2+Fe3+2O4 | 57.23% | Cubanite (57.24 %) |
Arsenolite | As2O3 | 55.00% | Claudetite (55.00 %) |
Malachite | Cu2(CO3)(OH)2 | 54.65% | Covellite (54.66 %) |
Barbosalite | Fe2+Fe3+2(PO4)2(OH)2 | 53.84% | Tavorite (53.85 %) |
Bermanite | Mn2+Mn3+2(PO4)2(OH)2 · 4H2O | 51.28% | Tavorite (51.28 %) |
Almandine | Fe2+3Al2(SiO4)3 | 50.63% | Laueite (50.63 %) |
Torbernite | Cu(UO2)2(PO4)2 · 12H2O | 50.47% | Phosphuranylite (50.48 %) |
Chalcocite | Cu2S | 50.30% | Covellite (50.30 %) |
Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O | 50.00% | Phosphuranylite (50.00 %) |
Fairfieldite | Ca2Mn2+(PO4)2 · 2H2O | 50.00% | Roscherite (50.00 %) |
Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) | 41.29% | Greifensteinite (51.61 %) |
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.