Predictive Mineralogy
Possible unrecorded species at Pyin-Oo-Lwin District, Mandalay Region, Myanmar
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 |
|---|---|---|---|
| Nepheline | Na3K(Al4Si4O16) | 99.17% | Aegirine-augite (50.72 %), Cancrinite (85.34 %), Haüyne (58.10 %), Sodalite (72.78 %) |
| Bismuth | Bi | 93.77% | Bismite (59.17 %), Joséite-A (84.75 %) |
| Bismuthinite | Bi2S3 | 92.54% | Bismite (60.00 %), Joséite-A (81.36 %) |
| Spodumene | LiAlSi2O6 | 58.54% | Montebrasite (58.55 %) |
| Joséite-B | Bi4Te2S | 54.23% | Joséite-A (54.24 %) |
| Arsenopyrite | FeAsS | 54.23% | Joséite-A (67.80 %) |
| Tantalite-(Mn) | Mn2+Ta2O6 | 52.38% | Stibiotantalite (52.38 %) |
| Tellurium | Te | 51.51% | Tellurite (51.52 %) |
| Trona | Na3H(CO3)2 · 2H2O | 50.00% | Shortite (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.