Predictive Mineralogy
Possible unrecorded species at Central Sudetes, Czech Republic/Poland
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% | Earlshannonite (100.00 %), Phosphoferrite (52.94 %), Rosemaryite (55.56 %), Whitmoreite (78.57 %) |
Parisite-(Ce) | CaCe2(CO3)3F2 | 100.00% | Hydropyrochlore (100.00 %) |
Rockbridgeite | Fe2+Fe3+4(PO4)3(OH)5 | 99.99% | Earlshannonite (86.67 %), Hureaulite (51.43 %), Kryzhanovskite (53.85 %), Mitridatite (51.66 %), Phosphoferrite (61.76 %), Rosemaryite (55.56 %), Serrabrancaite (66.67 %), Stanĕkite (64.29 %), Whitmoreite (78.57 %) |
Phosphosiderite | FePO4 · 2H2O | 99.89% | Earlshannonite (73.33 %), Hureaulite (55.00 %), Kryzhanovskite (56.41 %), Phosphoferrite (58.82 %), Serrabrancaite (88.89 %), Whitmoreite (57.14 %) |
Taenite | (Fe,Ni) | 98.18% | Daubréelite (66.87 %), Iron (59.58 %), Schreibersite (69.77 %), Troilite (55.20 %) |
Eosphorite | Mn2+Al(PO4)(OH)2 · H2O | 97.26% | Dickinsonite-(KMnNa) (62.07 %), Earlshannonite (53.33 %), Fairfieldite (56.79 %), Stanĕkite (64.29 %) |
Hessite | Ag2Te | 96.00% | Pilsenite (59.42 %), Rucklidgeite (58.02 %), Tellurium (51.48 %), Tellurobismuthite (51.61 %) |
Strengite | FePO4 · 2H2O | 95.76% | Earlshannonite (73.33 %), Serrabrancaite (66.67 %), Whitmoreite (52.38 %) |
Strunzite | Mn2+Fe3+2(PO4)2(OH)2 · 6H2O | 94.28% | Earlshannonite (80.00 %), Whitmoreite (71.43 %) |
Zinkenite | Pb9Sb22S42 | 93.74% | Fülöppite (69.70 %), Plagionite (53.10 %), Twinnite (56.00 %) |
Efremovite | (NH4)2Mg2(SO4)3 | 92.85% | Ammonioalunite (50.00 %), Godovikovite (57.14 %), Kladnoite (66.67 %) |
Lazulite | MgAl2(PO4)2(OH)2 | 92.59% | Ferrowyllieite (66.67 %), Rosemaryite (55.56 %), Wyllieite (50.00 %) |
Laueite | Mn2+Fe3+2(PO4)2(OH)2 · 8H2O | 90.47% | Earlshannonite (80.00 %), Whitmoreite (52.38 %) |
Leucophosphite | KFe3+2(PO4)2(OH) · 2H2O | 89.62% | Earlshannonite (53.33 %), Serrabrancaite (55.56 %), Stanĕkite (50.00 %) |
Montebrasite | LiAl(PO4)(OH) | 89.57% | Dickinsonite-(KMnNa) (51.72 %), Eucryptite (51.43 %), Rosemaryite (55.56 %) |
Frondelite | Mn2+Fe3+4(PO4)3(OH)5 | 88.88% | Earlshannonite (66.67 %), Serrabrancaite (66.67 %) |
Bermanite | Mn2+Mn3+2(PO4)2(OH)2 · 4H2O | 84.44% | Earlshannonite (53.33 %), Serrabrancaite (66.67 %) |
Rhodochrosite | MnCO3 | 84.44% | Fluorcalcioroméite (53.33 %), Natrophilite (66.67 %) |
Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O | 84.31% | Metauranopilite (66.67 %), Sengierite (52.94 %) |
Kainosite-(Y) | Ca2(Y,Ce)2(Si4O12)(CO3) · H2O | 83.33% | Cascandite (66.67 %), Hingganite-(Ce) (50.00 %) |
Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O | 81.17% | Earlshannonite (60.00 %), Sengierite (52.94 %) |
Voltaite | K2Fe2+5Fe3+3Al(SO4)12 · 18H2O | 80.51% | Millosevichite (54.55 %), Pyracmonite (57.14 %) |
Childrenite | Fe2+Al(PO4)(OH)2 · H2O | 79.25% | Earlshannonite (53.33 %), Rosemaryite (55.56 %) |
Altaite | PbTe | 72.83% | Rucklidgeite (72.84 %) |
Metavoltine | K2Na6Fe2+Fe3+6O2(SO4)12 · 18H2O | 71.42% | Pyracmonite (71.43 %) |
Stannite | Cu2FeSnS4 | 68.29% | Teallite (68.29 %) |
Geocronite | Pb14Sb6S23 | 68.00% | Twinnite (68.00 %) |
Cacoxenite | Fe3+24AlO6(PO4)17(OH)12 · 75H2O | 66.66% | Earlshannonite (66.67 %) |
Stewartite | Mn2+Fe3+2(PO4)2(OH)2 · 8H2O | 66.66% | Earlshannonite (66.67 %) |
Tyuyamunite | Ca(UO2)2(VO4)2 · 5-8H2O | 66.66% | Metauranopilite (66.67 %) |
Uranopilite | (UO2)6(SO4)O2(OH)6 · 14H2O | 66.66% | Metauranopilite (66.67 %) |
Braunite | Mn2+Mn3+6(SiO4)O8 | 66.66% | Fluorcalcioroméite (66.67 %) |
Rhodonite | CaMn3Mn[Si5O15] | 66.66% | Fluorcalcioroméite (66.67 %) |
Barbosalite | Fe2+Fe3+2(PO4)2(OH)2 | 66.66% | Serrabrancaite (66.67 %) |
Babingtonite | Ca2(Fe,Mn)FeSi5O14(OH) | 66.66% | Cascandite (66.67 %) |
Jervisite | NaSc3+Si2O6 | 66.66% | Cascandite (66.67 %) |
Kristiansenite | Ca4Sc2Sn2(Si2O7)2(Si2O6OH)2 | 66.66% | Cascandite (66.67 %) |
Tiemannite | HgSe | 63.63% | Antimonselite (63.64 %) |
Hausmannite | Mn2+Mn3+2O4 | 60.00% | Fluorcalcioroméite (60.00 %) |
Kutnohorite | CaMn2+(CO3)2 | 60.00% | Fluorcalcioroméite (60.00 %) |
Bayldonite | PbCu3(AsO4)2(OH)2 | 58.82% | Arsenogorceixite (58.82 %) |
Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 58.82% | Arsenogorceixite (58.82 %) |
Olivenite | Cu2(AsO4)(OH) | 58.82% | Arsenogorceixite (58.82 %) |
Linarite | PbCu(SO4)(OH)2 | 58.33% | Cesàrolite (58.33 %) |
Kremersite | (NH4,K)2[Fe3+Cl5(H2O)] | 57.14% | Pyracmonite (57.14 %) |
Sabieite | (NH4)Fe3+(SO4)2 | 57.14% | Pyracmonite (57.14 %) |
Picropharmacolite | Ca4Mg(AsO4)2(HAsO4)2 · 11H2O | 57.14% | Brassite (57.14 %) |
Cubanite | CuFe2S3 | 56.27% | Valleriite (56.27 %) |
Gustavite | AgPbBi3S6 | 56.25% | Vikingite (56.25 %) |
Alabandite | MnS | 55.88% | Oldhamite (55.88 %) |
Cyrilovite | NaFe3+3(PO4)2(OH)4 · 2H2O | 55.55% | Serrabrancaite (55.56 %) |
Tavorite | LiFe3+(PO4)(OH) | 55.55% | Serrabrancaite (55.56 %) |
Polyhalite | K2Ca2Mg(SO4)4 · 2H2O | 55.31% | Langbeinite (55.32 %) |
Jahnsite-(CaMnFe) | {Ca}{Mn2+}{Fe2+2}{Fe3+2}(PO4)4(OH)2 · 8H2O | 53.33% | Earlshannonite (53.33 %) |
Jahnsite-(CaMnMn) | {Ca}{Mn2+}{Mn2+2}{Fe3+2}(PO4)4(OH)2 · 8H2O | 53.33% | Earlshannonite (53.33 %) |
Carminite | PbFe3+2(AsO4)2(OH)2 | 52.94% | Arsenogorceixite (52.94 %) |
Philipsbornite | PbAl3(AsO4)(AsO3OH)(OH)6 | 52.94% | Arsenogorceixite (52.94 %) |
Kieserite | MgSO4 · H2O | 51.06% | Langbeinite (51.06 %) |
Wulfenite | Pb(MoO4) | 50.13% | Vanadinite (50.14 %) |
Maucherite | Ni11As8 | 50.00% | Godlevskite (50.00 %) |
Ludlamite | Fe2+3(PO4)2 · 4H2O | 50.00% | Phosphoferrite (50.00 %) |
Larnite | Ca2SiO4 | 50.00% | Srebrodolskite (50.00 %) |
Dufrénite | Ca0.5Fe2+Fe3+5(PO4)4(OH)6 · 2H2O | 50.00% | Stanĕkite (50.00 %) |
Lipscombite | Fe2+Fe3+2(PO4)2(OH)2 | 50.00% | Stanĕkite (50.00 %) |
Parasymplesite | Fe2+3(AsO4)2 · 8H2O | 50.00% | Brassite (50.00 %) |
Pharmacolite | Ca(HAsO4) · 2H2O | 50.00% | Brassite (50.00 %) |
Rauenthalite | Ca3(AsO4)2 · 10H2O | 50.00% | Brassite (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.