Predictive Mineralogy
Possible unrecorded species at Le Ravaner, Pegmatite field, Collioure, Céret, Pyrénées-Orientales, Occitanie, France
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 | 99.99% | Almandine (70.46 %), Andalusite (59.24 %), Diopside (51.68 %), Ferro-pargasite (62.50 %), Grossular (59.42 %), Hedenbergite (68.23 %), Muscovite (80.32 %), Schorl (81.37 %), Vesuvianite (53.96 %) |
Calcite | CaCO3 | 96.89% | Diopside (54.07 %), Grossular (59.86 %), Hedenbergite (60.34 %), Vesuvianite (57.54 %) |
Magnetite | Fe2+Fe3+2O4 | 81.09% | Ferro-pargasite (55.56 %), Hedenbergite (57.46 %) |
Pyrite | FeS2 | 76.17% | Hedenbergite (52.35 %), Muscovite (50.01 %) |
Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) | 51.38% | Ferro-pargasite (51.39 %) |
Titanite | CaTi(SiO4)O | 41.11% | Ferro-pargasite (51.39 %) |
Chalcopyrite | CuFeS2 | 40.85% | Hedenbergite (51.07 %) |
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.