Predictive Mineralogy
Possible unrecorded species at Alay Mountains, Asia
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 |
|---|---|---|---|
| Natrolite | Na2Al2Si3O10 路 2H2O | 99.99% | Epididymite (67.09 %), Fluorcaphite (71.43 %), Kentbrooksite (52.17 %), Kupletskite (65.00 %), Leucophanite (81.54 %), Mosandrite-(Ce) (54.69 %), Neptunite (61.82 %), Nordite-(Ce) (62.50 %), Perraultite (57.14 %), Rinkite-(Ce) (60.27 %), Tadzhikite-(Ce) (61.11 %) |
| Cerussite | PbCO3 | 99.93% | Alamosite (57.89 %), Anglesite (71.56 %), Descloizite (60.18 %), Hemimorphite (64.31 %), Mottramite (56.64 %), Smithsonite (55.69 %), Vanadinite (54.01 %), Willemite (57.56 %) |
| Rutile | TiO2 | 99.23% | Brookite (56.67 %), Chernovite-(Y) (52.63 %), Gasparite-(Ce) (53.57 %), Hydroxycalciopyrochlore (50.00 %), Hydroxylbastn盲site-(Nd) (55.56 %), Thorutite (63.64 %) |
| Monazite-(Ce) | Ce(PO4) | 97.80% | Chernovite-(Y) (54.39 %), Fluorcalciobritholite (57.14 %), Gasparite-(Ce) (60.71 %), Perraultite (71.43 %) |
| Catapleiite | Na2Zr(Si3O9) 路 2H2O | 96.48% | Fluorcaphite (57.14 %), Kentbrooksite (52.17 %), Kupletskite (60.00 %), Perraultite (57.14 %) |
| Aenigmatite | Na4[Fe2+10Ti2]O4[Si12O36] | 90.38% | Tuhualite (75.00 %), Turkestanite (61.54 %) |
| Lorenzenite | Na2Ti2(Si2O6)O3 | 85.71% | Fluorcaphite (71.43 %), Nordite-(Ce) (50.00 %) |
| Pollucite | (Cs,Na)2(Al2Si4O12) 路 2H2O | 83.33% | Sokolovaite (83.33 %) |
| Rhodochrosite | MnCO3 | 79.16% | Hejtmanite (58.33 %), Sugilite (50.00 %) |
| Loparite-(Ce) | (Na,REE)2Ti2O6 | 78.57% | Fluorcaphite (57.14 %), Nordite-(Ce) (50.00 %) |
| Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 | 76.92% | Tuhualite (50.00 %), Turkestanite (53.85 %) |
| Anatase | TiO2 | 76.21% | Brookite (76.21 %) |
| Uranophane | Ca(UO2)2(SiO3OH)2 路 5H2O | 75.00% | Haiweeite (75.00 %) |
| Serandite | NaMn2+2Si3O8(OH) | 75.00% | Nordite-(Ce) (50.00 %), Sugilite (50.00 %) |
| Murmanite | Na2Ti2(Si2O7)O2 路 2H2O | 71.42% | Fluorcaphite (71.43 %) |
| Beryl | Be3Al2(Si6O18) | 70.83% | Columbite-(Mn) (70.83 %) |
| Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) | 66.66% | Sokolovaite (66.67 %) |
| W枚hlerite | Na2Ca4ZrNb(Si2O7)2O3F | 66.66% | Tadzhikite-(Ce) (66.67 %) |
| Colusite | Cu13VAs3S16 | 66.66% | Velikite (66.67 %) |
| Braunite | Mn2+Mn3+6(SiO4)O8 | 64.28% | Sugilite (64.29 %) |
| Narsarsukite | Na4(Ti,Fe)2[Si8O20](O,OH,F)2 | 62.50% | Tuhualite (62.50 %) |
| Nahcolite | NaHCO3 | 60.00% | Reedmergnerite (60.00 %) |
| Acanthite | Ag2S | 57.14% | Gruzdevite (57.14 %) |
| Labuntsovite-Mn | Na4K4(Ba,K)2Mn2+(Ti,Nb)8(Si4O12)4(O,OH)8 路 10-12H2O | 57.14% | Fluorcaphite (57.14 %) |
| Lamprophyllite | (Na,Mn2+)3(Sr,Na)2(Ti,Fe3+)3(Si2O7)2O2(OH,O,F)2 | 57.14% | Fluorcaphite (57.14 %) |
| Villiaumite | NaF | 57.14% | Fluorcaphite (57.14 %) |
| Lemmleinite-K | K2(Ti,Nb)2(Si4O12)(OH,O)2 路 4H2O | 57.14% | Fluorcaphite (57.14 %) |
| Ecdemite | Pb6Cl4(As2O7) | 55.55% | Shakhovite (55.56 %) |
| Xenotime-(Y) | Y(PO4) | 54.38% | Chernovite-(Y) (54.39 %) |
| Sanbornite | Ba2(Si4O10) | 52.94% | Bazirite (52.94 %) |
| Grossular | Ca3Al2(SiO4)3 | 52.38% | Ekanite (52.38 %) |
| Prehnite | Ca2Al2Si3O10(OH)2 | 50.26% | Datolite (50.26 %) |
| Wulfenite | Pb(MoO4) | 50.13% | Vanadinite (50.14 %) |
| Parauranophane | Ca(UO2)2(SiO3OH)2 路 5H2O | 50.00% | Haiweeite (50.00 %) |
| Belovite-(Ce) | NaCeSr3(PO4)3F | 50.00% | Nordite-(Ce) (50.00 %) |
| Chkalovite | Na2BeSi2O6 | 50.00% | Nordite-(Ce) (50.00 %) |
| Magnesio-arfvedsonite | {Na}{Na2}{Mg4Fe3+}(Si8O22)(OH)2 | 50.00% | Nordite-(Ce) (50.00 %) |
| Manganoneptunite | KNa2Li(Mn2+)2Ti2[Si4O12]2 | 50.00% | Nordite-(Ce) (50.00 %) |
| Steenstrupine-(Ce) | Na14Mn2+2Fe3+2Ce6Zr(Si6O18)2(PO4)6(PO3OH)(OH)2 路 2H2O | 50.00% | Nordite-(Ce) (50.00 %) |
| Trona | Na3H(CO3)2 路 2H2O | 50.00% | Shortite (50.00 %) |
| Hausmannite | Mn2+Mn3+2O4 | 50.00% | Sugilite (50.00 %) |
| Opal | SiO2 路 nH2O | 50.00% | Tuhualite (50.00 %) |
| Tiemannite | HgSe | 45.71% | Gruzdevite (57.14 %) |
| Coloradoite | HgTe | 40.00% | Tvalchrelidzeite (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.