Predictive Mineralogy
Possible unrecorded species at Etang de Lers, Col d'Agnès, Le Port, Saint-Girons, Ariège, 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 |
---|---|---|---|
Pyrite | FeS2 | 99.96% | Calcite (51.16 %), Chalcopyrite (75.16 %), Galena (66.84 %), Muscovite (50.01 %), Pyrrhotite (80.12 %), Pentlandite (58.72 %), Rockbridgeite (52.19 %), Rutile (52.79 %) |
Albite | Na(AlSi3O8) | 85.50% | Alluaudite (66.98 %), Microcline (56.11 %) |
Sphalerite | ZnS | 74.00% | Chalcopyrite (50.66 %), Galena (65.95 %), Pyrrhotite (55.40 %) |
Heterosite | (Fe3+,Mn3+)PO4 | 55.66% | Alluaudite (55.66 %) |
Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 | 55.62% | Kaersutite (55.63 %) |
Beraunite | Fe3+6(PO4)4O(OH)4 · 6H2O | 54.82% | Rockbridgeite (54.82 %) |
Lead | Pb | 54.54% | Anyuiite (54.55 %) |
Triphylite | LiFe2+PO4 | 52.83% | Alluaudite (66.04 %) |
Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 51.88% | Alluaudite (51.89 %) |
Strengite | FePO4 · 2H2O | 50.43% | Rockbridgeite (50.44 %) |
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.