Predictive Mineralogy
Possible unrecorded species at Morrison Cu-Au deposit, Granisle, Omineca Mining Division, British Columbia, 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 |
---|---|---|---|
Quartz | SiO2 | 99.99% | Actinolite (69.88 %), Anhydrite (50.95 %), Arsenopyrite (80.07 %), Bornite (66.21 %), Boulangerite (82.13 %), Calcite (62.43 %), Chalcocite (63.99 %), Chalcopyrite (67.26 %), Covellite (76.39 %), Epidote (69.84 %), Galena (65.16 %), Geocronite (76.43 %), Hematite (62.61 %), Jarosite (68.17 %), Kaolinite (71.35 %), Magnetite (50.54 %), Marcasite (70.46 %), Molybdenite (66.37 %), Muscovite (80.32 %), Pyrite (67.27 %), Pyrrhotite (67.51 %), Sphalerite (67.53 %), Stilpnomelane (62.50 %) |
Malachite | Cu2(CO3)(OH)2 | 80.13% | Chalcocite (56.20 %), Covellite (54.66 %) |
Bournonite | PbCuSbS3 | 53.50% | Geocronite (53.50 %) |
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.