Predictive Mineralogy
Possible unrecorded species at Corundum occurrence, Kawai-cho-tsukigase, Hida City, Gifu Prefecture, Japan
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 | 99.98% | Epidote (69.84 %), Lepidocrocite (78.01 %), Muscovite (80.32 %), Prehnite (64.07 %), Rutile (72.22 %), Titanite (65.16 %), Zircon (64.02 %) |
Pyrite | FeS2 | 97.06% | Epidote (56.37 %), Lepidocrocite (71.47 %), Muscovite (50.01 %), Rutile (52.79 %) |
Calcite | CaCO3 | 96.04% | Epidote (51.60 %), Lepidocrocite (55.87 %), Prehnite (61.24 %), Titanite (52.17 %) |
Goethite | Ξ±-Fe3+O(OH) | 76.37% | Lepidocrocite (76.37 %) |
Hematite | Fe2O3 | 55.12% | Lepidocrocite (55.13 %) |
Chalcopyrite | CuFeS2 | 46.71% | Lepidocrocite (58.40 %) |
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.