Predictive Mineralogy
Possible unrecorded species at Irkutsk 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 |
|---|---|---|---|
| Moncheite | Pt(Te,Bi)2 | 99.88% | Kotulskite (61.68 %), Merenskyite (50.00 %), Michenerite (53.25 %), Polarite (58.82 %), Sobolevskite (58.57 %), Taimyrite (64.71 %), Tarkianite (50.00 %), Urvantsevite (57.14 %) |
| Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 99.04% | Elbaite (59.66 %), Eucryptite (51.43 %), Lithiophilite (52.66 %), Montebrasite (54.27 %), Pollucite (54.27 %), Scorzalite (50.70 %) |
| Rhodochrosite | MnCO3 | 97.19% | Alabandite (54.55 %), Kukharenkoite-(Ce) (50.00 %), Kutnohorite (69.18 %), Vuorelainenite (60.00 %) |
| Atokite | (Pd,Pt)3Sn | 92.88% | Polarite (52.94 %), Taimyrite (64.71 %), Urvantsevite (57.14 %) |
| Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 | 92.38% | Barytolamprophyllite (55.56 %), Chlorbartonite (57.14 %), Villiaumite (60.00 %) |
| Zvyagintsevite | Pd3Pb | 89.91% | Taimyrite (52.94 %), Tarkianite (50.00 %), Urvantsevite (57.14 %) |
| Colemanite | Ca[B3O4(OH)3] · H2O | 85.71% | Ginorite (54.55 %), Priceite (68.57 %) |
| Osmium | (Os,Ir,Ru) | 85.55% | Ruthenium (69.35 %), Tulameenite (52.86 %) |
| Lamprophyllite | (Na,Mn2+)3(Sr,Na)2(Ti,Fe3+)3(Si2O7)2O2(OH,O,F)2 | 84.12% | Barytolamprophyllite (62.96 %), Chlorbartonite (57.14 %) |
| Taenite | (Fe,Ni) | 81.89% | Iron (59.58 %), Troilite (55.20 %) |
| Rankinite | Ca3Si2O7 | 81.81% | Kilchoanite (81.82 %) |
| Spessartine | Mn2+3Al2(SiO4)3 | 80.00% | Rynersonite (50.00 %), Vuorelainenite (60.00 %) |
| Rustenburgite | (Pt,Pd)3Sn | 79.83% | Taimyrite (52.94 %), Urvantsevite (57.14 %) |
| Lorenzenite | Na2Ti2(Si2O6)O3 | 78.57% | Chlorbartonite (57.14 %), Kukharenkoite-(Ce) (50.00 %) |
| Franckeite | Fe2+(Pb,Sn2+)6Sn4+2Sb2S14 | 76.92% | Cylindrite (76.92 %) |
| Catapleiite | Na2Zr(Si3O9) · 2H2O | 76.19% | Ancylite-(La) (52.38 %), Kukharenkoite-(Ce) (50.00 %) |
| Tiemannite | HgSe | 73.33% | Hakite-(Hg) (73.33 %) |
| Tobermorite | Ca4Si6O17(H2O)2 · (Ca · 3H2O) | 72.72% | Kilchoanite (72.73 %) |
| Antigorite | Mg3(Si2O5)(OH)4 | 71.42% | Kulkeite (71.43 %) |
| Cotunnite | PbCl2 | 71.42% | Parascandolaite (71.43 %) |
| Sudburyite | PdSb | 68.75% | Naldrettite (68.75 %) |
| Palladium | (Pd,Pt) | 68.42% | Rhodium (68.42 %) |
| Stannite | Cu2FeSnS4 | 65.38% | Cylindrite (65.38 %) |
| Vivianite | Fe2+Fe2+2(PO4)2 · 8H2O | 64.00% | Santabarbaraite (64.00 %) |
| Kainosite-(Y) | Ca2(Y,Ce)2(Si4O12)(CO3) · H2O | 62.50% | Aluminocerite-(CeCa) (62.50 %) |
| Jamesonite | Pb4FeSb6S14 | 61.53% | Cylindrite (61.54 %) |
| Wurtzite | (Zn,Fe)S | 61.53% | Cylindrite (61.54 %) |
| Iridium | (Ir,Os,Ru) | 61.29% | Ruthenium (61.29 %) |
| Eskebornite | CuFeSe2 | 60.00% | Hakite-(Hg) (60.00 %) |
| Donnayite-(Y) | NaCaSr3Y(CO3)6 · 3H2O | 60.00% | Kukharenkoite-(Ce) (60.00 %) |
| Chlormayenite | Ca12Al14O32[◻4Cl2] | 60.00% | Calcio-olivine (60.00 %) |
| Srebrodolskite | Ca2Fe3+2O5 | 60.00% | Calcio-olivine (60.00 %) |
| Hydrocalumite | Ca4Al2(OH)12(Cl,CO3,OH)2 · 4H2O | 58.33% | Kerimasite (58.33 %) |
| Lakargiite | Ca(Zr,Sn,Ti)O3 | 58.33% | Kerimasite (58.33 %) |
| Cinnabar | HgS | 57.89% | Luanheite (57.89 %) |
| Anthophyllite | ◻{Mg2}{Mg5}(Si8O22)(OH)2 | 57.14% | Kulkeite (57.14 %) |
| Magnesio-hornblende | ◻Ca2(Mg4Al)(Si7Al)O22(OH)2 | 57.14% | Kulkeite (57.14 %) |
| Steenstrupine-(Ce) | Na14Mn2+2Fe3+2Ce6Zr(Si6O18)2(PO4)6(PO3OH)(OH)2 · 2H2O | 57.14% | Chlorbartonite (57.14 %) |
| Aeschynite-(Ce) | (Ce,Ca,Fe,Th)(Ti,Nb)2(O,OH)6 | 57.14% | Nioboaeschynite-(Ce) (57.14 %) |
| Sanidine | K(AlSi3O8) | 57.14% | Afghanite (57.14 %) |
| Majakite | PdNiAs | 57.14% | Urvantsevite (57.14 %) |
| Mooihoekite | Cu9Fe9S16 | 57.14% | Urvantsevite (57.14 %) |
| Paolovite | Pd2Sn | 57.14% | Urvantsevite (57.14 %) |
| Plumbopalladinite | Pd3Pb2 | 57.14% | Urvantsevite (57.14 %) |
| Stannopalladinite | (Pd,Cu)3Sn | 57.14% | Urvantsevite (57.14 %) |
| Talnakhite | Cu9(Fe,Ni)8S16 | 57.14% | Urvantsevite (57.14 %) |
| Gearksutite | Ca[Al(F,OH)5(H2O)] | 57.14% | Parascandolaite (57.14 %) |
| Matlockite | PbFCl | 57.14% | Parascandolaite (57.14 %) |
| Sbacchiite | Ca2AlF7 | 57.14% | Parascandolaite (57.14 %) |
| Stibnite | Sb2S3 | 56.41% | Antimony (56.42 %) |
| Parisite-(Ce) | CaCe2(CO3)3F2 | 55.00% | Cordylite-(Ce) (55.00 %) |
| Shortite | Na2Ca2(CO3)3 | 55.00% | Neighborite (55.00 %) |
| Thénardite | Na2SO4 | 53.84% | Northupite (53.85 %) |
| Trona | Na3H(CO3)2 · 2H2O | 53.84% | Northupite (53.85 %) |
| Eucairite | AgCuSe | 53.33% | Hakite-(Hg) (53.33 %) |
| Ferroselite | FeSe2 | 53.33% | Hakite-(Hg) (53.33 %) |
| Anatase | TiO2 | 51.40% | Synchysite-(Ce) (51.41 %) |
| Boulangerite | Pb5Sb4S11 | 50.00% | Cylindrite (50.00 %) |
| Isomertieite | Pd11Sb2As2 | 50.00% | Tarkianite (50.00 %) |
| Melonite | NiTe2 | 50.00% | Tarkianite (50.00 %) |
| Kotoite | Mg3[BO3]2 | 50.00% | Sakhaite (50.00 %) |
| Kieserite | MgSO4 · H2O | 50.00% | Sulfoborite (50.00 %) |
| Hingganite-(Y) | (Y,REE,Ca)2(◻,Fe2+)Be2[SiO4]2(OH)2 | 50.00% | Aluminocerite-(CeCa) (50.00 %) |
| Wulfenite | Pb(MoO4) | 50.00% | Aluminocerite-(CeCa) (50.00 %) |
| Rhodonite | CaMn3Mn[Si5O15] | 50.00% | Vuorelainenite (50.00 %) |
| Ewaldite | Ba(Na,Ca,Y,Ce,K)(CO3)2 · 2.6H2O | 50.00% | Kukharenkoite-(Ce) (50.00 %) |
| Hilairite | Na2Zr[SiO3]3 · 3H2O | 50.00% | Kukharenkoite-(Ce) (50.00 %) |
| Labuntsovite-Mn | Na4K4(Ba,K)2Mn2+(Ti,Nb)8(Si4O12)4(O,OH)8 · 10-12H2O | 50.00% | Kukharenkoite-(Ce) (50.00 %) |
| Tridymite | SiO2 | 50.00% | Calcio-olivine (50.00 %) |
| Ammineite | [CuCl2(NH3)2] | 45.71% | Parascandolaite (57.14 %) |
| Bukovite | (Cu3Fe)Σ4Tl2Se4 | 42.66% | Hakite-(Hg) (53.33 %) |
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.