Predictive Mineralogy
Possible unrecorded species at Kiyokawa 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 | 99.06% | Alleghanyite (53.33 %), Hausmannite (51.00 %), Jacobsite (52.02 %), Pyroxmangite (53.01 %), Rhodochrosite (50.69 %), Sussexite (63.33 %) |
Pyrite | FeS2 | 93.85% | Pyroxmangite (52.41 %), Rhodochrosite (56.95 %), Sussexite (70.00 %) |
Baryte | BaSO4 | 62.66% | Sussexite (56.67 %), Wiserite (50.00 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 54.50% | Spessartine (54.51 %) |
Magnetite | Fe2+Fe3+2O4 | 50.00% | Sussexite (50.00 %) |
Sphalerite | ZnS | 45.33% | Sussexite (56.67 %) |
Galena | PbS | 40.00% | Sussexite (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.