Predictive Mineralogy
Possible unrecorded species at U starého Čihadla pegmatite, Biskupice-Pulkov, Třebíč District, Vysočina Region, Czech Republic
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 | 99.99% | Albite (78.81 %), Cassiterite (58.88 %), Elbaite (78.47 %), Fluorite (66.12 %), Microcline (81.52 %), Orthoclase (76.14 %), Polylithionite (66.67 %), Rutile (72.22 %), Tantalite-(Mn) (84.23 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 98.33% | Albite (52.80 %), Elbaite (62.03 %), Microcline (61.50 %), Tantalite-(Mn) (75.93 %) |
Beryl | Be3Al2(Si6O18) | 71.68% | Elbaite (60.85 %), Tantalite-(Mn) (73.44 %) |
Zircon | Zr(SiO4) | 66.94% | Polylithionite (66.67 %), Tantalite-(Mn) (51.04 %) |
Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 59.66% | Elbaite (59.66 %) |
Aegirine | NaFe3+Si2O6 | 58.33% | Polylithionite (58.33 %) |
Pyrite | FeS2 | 52.78% | Rutile (52.79 %) |
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.