Predictive Mineralogy
Possible unrecorded species at Tari-Misaka Ultramafic Complex, Tottori 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 | 99.45% | Diopside (51.68 %), Cordierite (64.23 %), Ilmenite (52.06 %), Magnetite (50.54 %), Rutile (72.22 %), Talc (52.15 %) |
Calcite | CaCO3 | 90.77% | Diopside (54.07 %), Lizardite (54.44 %), Phlogopite (55.90 %) |
Pyrite | FeS2 | 52.78% | Rutile (52.79 %) |
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.