Predictive Mineralogy
Possible unrecorded species at Okutama mine, Okutama-cho, Nishitama district, Tokyo Metropolis, 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 |
|---|---|---|---|
| Calcite | CaCO3 | 99.84% | Caryopilite (70.33 %), Ganophyllite (76.00 %), Hausmannite (51.00 %), Manganosite (54.88 %), Neotocite (50.23 %), Rhodochrosite (50.69 %), Siegenite (60.07 %) |
| Chalcopyrite | CuFeS2 | 73.01% | Pyrite (51.72 %), Siegenite (81.91 %) |
| Baryte | BaSO4 | 66.06% | Ganophyllite (58.00 %), Manganosite (58.54 %) |
| Galena | PbS | 55.15% | Siegenite (68.94 %) |
| Sphalerite | ZnS | 55.15% | Siegenite (68.94 %) |
| Braunite | Mn2+Mn3+6(SiO4)O8 | 54.00% | Ganophyllite (54.00 %) |
| Spessartine | Mn2+3Al2(SiO4)3 | 52.55% | Tephroite (52.55 %) |
| Millerite | NiS | 51.19% | Siegenite (51.19 %) |
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.