Predictive Mineralogy
Possible unrecorded species at Montemor-o-Novo, Évora, Portugal
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 |
---|---|---|---|
Gypsum | CaSO4 · 2H2O | 91.91% | Copiapite (56.84 %), Lavendulan (59.65 %), Melanterite (53.56 %) |
Bismuth | Bi | 75.18% | Hedleyite (75.19 %) |
Olivenite | Cu2(AsO4)(OH) | 58.47% | Lavendulan (58.48 %) |
Diopside | CaMgSi2O6 | 52.96% | Vesuvianite (52.97 %) |
Cuprite | Cu2O | 52.50% | Plancheite (52.50 %) |
Brochantite | Cu4(SO4)(OH)6 | 50.29% | Lavendulan (50.29 %) |
Hessite | Ag2Te | 47.65% | Altaite (59.57 %) |
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.