Predictive Mineralogy
Possible unrecorded species at Voron'i Tundry, Murmansk Oblast, Russia
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 |
---|---|---|---|
Beraunite | Fe3+6(PO4)4O(OH)4 · 6H2O | 100.00% | Gordonite (56.52 %), Jahnsite-(CaMnFe) (100.00 %), Kingsmountite (70.59 %), Laueite (64.56 %), Lithiophosphate (57.14 %), Lun'okite (66.67 %), Mangangordonite (100.00 %) |
Calcite | CaCO3 | 99.99% | Acanthite (51.71 %), Analcime (57.00 %), Arseniosiderite (65.04 %), Bavenite (51.90 %), Boulangerite (52.73 %), Calaverite (51.83 %), Cervelleite (50.00 %), Cobaltite (51.81 %), Diaphorite (54.14 %), Diopside (54.07 %), Dyscrasite (63.35 %), Epidote (51.60 %), Fizélyite (54.84 %), Greenockite (70.86 %), Hydroxycalciopyrochlore (72.22 %), Kolfanite (71.43 %), Löllingite (51.02 %), Marcasite (60.67 %), Mckinstryite (69.44 %), Petzite (51.11 %), Ramdohrite (50.00 %), Rubicline (50.00 %), Semseyite (55.66 %), Stephanite (54.56 %), Symplesite (52.43 %), Ullmannite (56.15 %), Uytenbogaardtite (53.03 %) |
Rockbridgeite | Fe2+Fe3+4(PO4)3(OH)5 | 99.89% | Gordonite (52.17 %), Jahnsite-(CaMnFe) (83.33 %), Laueite (77.22 %), Mangangordonite (87.50 %), Mitridatite (51.66 %) |
Phosphosiderite | FePO4 · 2H2O | 98.98% | Jahnsite-(CaMnFe) (72.22 %), Laueite (70.89 %), Mangangordonite (87.50 %) |
Strengite | FePO4 · 2H2O | 98.87% | Jahnsite-(CaMnFe) (61.11 %), Kingsmountite (52.94 %), Laueite (50.63 %), Mangangordonite (87.50 %) |
Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | 98.80% | Fairfieldite (58.02 %), Jahnsite-(CaMnFe) (52.78 %), Laueite (51.90 %), Mangangordonite (87.50 %) |
Strunzite | Mn2+Fe3+2(PO4)2(OH)2 · 6H2O | 98.47% | Jahnsite-(CaMnFe) (66.67 %), Laueite (63.29 %), Mangangordonite (87.50 %) |
Heterosite | (Fe3+,Mn3+)PO4 | 98.41% | Jahnsite-(CaMnFe) (66.67 %), Laueite (62.03 %), Mangangordonite (87.50 %) |
Hureaulite | Mn2+5(PO3OH)2(PO4)2 · 4H2O | 98.07% | Fairfieldite (53.09 %), Jahnsite-(CaMnFe) (63.89 %), Laueite (54.43 %), Mangangordonite (75.00 %) |
Almandine | Fe2+3Al2(SiO4)3 | 97.80% | Fairfieldite (54.32 %), Jahnsite-(CaMnFe) (61.11 %), Laueite (50.63 %), Mangangordonite (75.00 %) |
Stibnite | Sb2S3 | 96.48% | Aurostibite (58.06 %), Fizélyite (51.61 %), Ramdohrite (62.50 %), Semseyite (53.77 %) |
Siderite | FeCO3 | 92.06% | Kolfanite (57.14 %), Laueite (50.63 %), Mangangordonite (62.50 %) |
Fluorite | CaF2 | 91.56% | Bavenite (53.29 %), Hydroxycalciopyrochlore (50.00 %), Polylithionite (63.89 %) |
Torbernite | Cu(UO2)2(PO4)2 · 12H2O | 88.88% | Jahnsite-(CaMnFe) (55.56 %), Mangangordonite (75.00 %) |
Childrenite | Fe2+Al(PO4)(OH)2 · H2O | 87.50% | Mangangordonite (87.50 %) |
Scorodite | Fe3+AsO4 · 2H2O | 84.32% | Arseniosiderite (57.52 %), Symplesite (63.11 %) |
Bismuthinite | Bi2S3 | 82.85% | Bismite (60.00 %), Kolfanite (57.14 %) |
Bournonite | PbCuSbS3 | 82.53% | Fizélyite (54.84 %), Semseyite (61.32 %) |
Miargyrite | AgSbS2 | 80.12% | Fizélyite (53.23 %), Ramdohrite (57.50 %) |
Malachite | Cu2(CO3)(OH)2 | 79.13% | Arseniosiderite (53.98 %), Covellite (54.66 %) |
Bermanite | Mn2+Mn3+2(PO4)2(OH)2 · 4H2O | 75.00% | Mangangordonite (75.00 %) |
Cacoxenite | Fe3+24AlO6(PO4)17(OH)12 · 75H2O | 75.00% | Mangangordonite (75.00 %) |
Frondelite | Mn2+Fe3+4(PO4)3(OH)5 | 75.00% | Mangangordonite (75.00 %) |
Opal | SiO2 · nH2O | 75.00% | Mangangordonite (75.00 %) |
Paravauxite | Fe2+Al2(PO4)2(OH)2 · 8H2O | 75.00% | Mangangordonite (75.00 %) |
Robertsite | Ca2Mn3+3(PO4)3O2 · 3H2O | 75.00% | Mangangordonite (75.00 %) |
Stewartite | Mn2+Fe3+2(PO4)2(OH)2 · 8H2O | 75.00% | Mangangordonite (75.00 %) |
Variscite | AlPO4 · 2H2O | 75.00% | Mangangordonite (75.00 %) |
Xanthoxenite | Ca4Fe3+2(PO4)4(OH)2 · 3H2O | 75.00% | Mangangordonite (75.00 %) |
Kastningite | (Mn2+,Fe2+,Mg)Al2(PO4)2(OH)2 · 8H2O | 75.00% | Mangangordonite (75.00 %) |
Cerussite | PbCO3 | 68.60% | Pyromorphite (68.61 %) |
Altaite | PbTe | 65.59% | Stützite (65.60 %) |
Thorite | Th(SiO4) | 64.44% | Hafnon (50.00 %), Hydroxycalciopyrochlore (61.11 %) |
Topaz | Al2(SiO4)(F,OH)2 | 63.15% | Fluornatromicrolite (63.16 %) |
Cryptomelane | K(Mn4+7Mn3+)O16 | 62.50% | Mangangordonite (62.50 %) |
Dufrénite | Ca0.5Fe2+Fe3+5(PO4)4(OH)6 · 2H2O | 62.50% | Mangangordonite (62.50 %) |
Messelite | Ca2Fe2+(PO4)2 · 2H2O | 62.50% | Mangangordonite (62.50 %) |
Stromeyerite | AgCuS | 59.72% | Mckinstryite (59.72 %) |
Aegirine | NaFe3+Si2O6 | 58.33% | Polylithionite (58.33 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 | 57.14% | Kolfanite (57.14 %) |
Conichalcite | CaCu(AsO4)(OH) | 57.14% | Kolfanite (57.14 %) |
Dolomite | CaMg(CO3)2 | 57.14% | Kolfanite (57.14 %) |
Pharmacosiderite | KFe3+4(AsO4)3(OH)4 · 6-7H2O | 57.14% | Kolfanite (57.14 %) |
Whitlockite | Ca9Mg(PO4)6(PO3OH) | 57.14% | Lithiophosphate (57.14 %) |
Crandallite | CaAl3(PO4)(PO3OH)(OH)6 | 52.17% | Gordonite (52.17 %) |
Sylvanite | AgAuTe4 | 51.20% | Stützite (51.20 %) |
Titanite | CaTi(SiO4)O | 50.51% | Bavenite (50.52 %) |
Chalcocite | Cu2S | 50.30% | Covellite (50.30 %) |
Earlshannonite | Mn2+Fe3+2(PO4)2(OH)2 · 4H2O | 50.00% | Mangangordonite (50.00 %) |
Ferrostrunzite | Fe2+Fe3+2(PO4)2(OH)2 · 6H2O | 50.00% | Mangangordonite (50.00 %) |
Graphite | C | 50.00% | Mangangordonite (50.00 %) |
Hydroxylapatite | Ca5(PO4)3(OH) | 50.00% | Mangangordonite (50.00 %) |
Jahnsite-(CaMnMn) | {Ca}{Mn2+}{Mn2+2}{Fe3+2}(PO4)4(OH)2 · 8H2O | 50.00% | Mangangordonite (50.00 %) |
Leucophosphite | KFe3+2(PO4)2(OH) · 2H2O | 50.00% | Mangangordonite (50.00 %) |
Lipscombite | Fe2+Fe3+2(PO4)2(OH)2 | 50.00% | Mangangordonite (50.00 %) |
Metaswitzerite | Mn2+3(PO4)2 · 4H2O | 50.00% | Mangangordonite (50.00 %) |
Phosphophyllite | Zn2Fe(PO4)2 · 4H2O | 50.00% | Mangangordonite (50.00 %) |
Whitmoreite | Fe2+Fe3+2(PO4)2(OH)2 · 4H2O | 50.00% | Mangangordonite (50.00 %) |
Hematite | Fe2O3 | 50.00% | Hydroxycalciopyrochlore (50.00 %) |
Monazite-(Ce) | Ce(PO4) | 40.00% | Mangangordonite (50.00 %) |
Baryte | BaSO4 | 40.00% | Ramdohrite (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.