Predictive Mineralogy
Possible unrecorded species at Nangalam pegmatite field, Dara-e-Pech District, Kunar, Afghanistan
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 | 99.15% | Albite (78.81 %), Spodumene (75.69 %), Wodginite (83.54 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 95.04% | Albite (52.80 %), Spodumene (62.28 %), Wodginite (72.15 %) |
Cassiterite | SnO2 | 72.15% | Wodginite (72.15 %) |
Beryl | Be3Al2(Si6O18) | 71.75% | Spodumene (59.27 %), Wodginite (74.68 %) |
Microcline | K(AlSi3O8) | 62.02% | Wodginite (62.03 %) |
Zircon | Zr(SiO4) | 40.50% | Wodginite (50.63 %) |
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.