Predictive Mineralogy
Possible unrecorded species at Dumont intrusion, Launay, Abitibi RCM, Abitibi-Témiscamingue, Québec, Canada
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 |
|---|---|---|---|
| Magnetite | Fe2+Fe3+2O4 | 98.20% | Awaruite (68.00 %), Coalingite (58.06 %), Heazlewoodite (67.73 %), Pentlandite (58.50 %) |
| Chalcopyrite | CuFeS2 | 86.86% | Paratacamite (50.00 %), Pentlandite (73.72 %) |
| Pyrite | FeS2 | 79.36% | Paratacamite (50.00 %), Pentlandite (58.72 %) |
| Pyrrhotite | Fe1-xS | 74.77% | Pentlandite (74.78 %) |
| Chromite | Fe2+Cr3+2O4 | 66.84% | Awaruite (57.00 %), Heazlewoodite (61.75 %) |
| Quartz | SiO2 | 63.15% | Paratacamite (63.16 %) |
| Atacamite | Cu2(OH)3Cl | 58.42% | Paratacamite (58.42 %) |
| Hydromagnesite | Mg5(CO3)4(OH)2 · 4H2O | 58.06% | Coalingite (58.06 %) |
| Malachite | Cu2(CO3)(OH)2 | 57.89% | Paratacamite (57.89 %) |
| Millerite | NiS | 52.98% | Heazlewoodite (52.99 %) |
| Calcite | CaCO3 | 52.63% | Paratacamite (52.63 %) |
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.