Predictive Mineralogy
Possible unrecorded species at Shin-Otani mine, Ukyou-ku, Kyoto City, Kyoto 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 | 98.02% | Pyrolusite (54.91 %), Rhodochrosite (69.08 %), Tephroite (54.74 %), Wiserite (68.75 %) |
Rhodonite | CaMn3Mn[Si5O15] | 91.05% | Tephroite (79.56 %), Wiserite (56.25 %) |
Hausmannite | Mn2+Mn3+2O4 | 81.25% | Wiserite (81.25 %) |
Jacobsite | Mn2+Fe3+2O4 | 75.00% | Wiserite (75.00 %) |
Pyrite | FeS2 | 56.95% | Rhodochrosite (56.95 %) |
Alleghanyite | Mn2+5(SiO4)2(OH)2 | 56.25% | Wiserite (56.25 %) |
Spessartine | Mn2+3Al2(SiO4)3 | 52.55% | Tephroite (52.55 %) |
Calcite | CaCO3 | 50.68% | Rhodochrosite (50.69 %) |
Sussexite | Mn2+BO2(OH) | 50.00% | Wiserite (50.00 %) |
Baryte | BaSO4 | 40.00% | Wiserite (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.