Predictive Mineralogy
Possible unrecorded species at Iraq
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 |
---|---|---|---|
Titanite | CaTi(SiO4)O | 96.58% | Baghdadite (54.55 %), Calzirtite (50.00 %), Hastingsite (50.85 %), Schorlomite (69.44 %) |
Andradite | Ca3Fe3+2(SiO4)3 | 94.53% | Baghdadite (63.64 %), Cuspidine (52.94 %), Schorlomite (68.06 %) |
Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 | 86.90% | Baghdadite (63.64 %), Foshagite (64.00 %) |
Torbernite | Cu(UO2)2(PO4)2 · 12H2O | 60.00% | Curienite (60.00 %) |
Cubanite | CuFe2S3 | 56.27% | Valleriite (56.27 %) |
Microcline | K(AlSi3O8) | 55.91% | Columbite-(Fe) (55.92 %) |
Tyuyamunite | Ca(UO2)2(VO4)2 · 5-8H2O | 53.33% | Metatyuyamunite (53.33 %) |
Brucite | Mg(OH)2 | 50.94% | Hydrotalcite (50.94 %) |
Silver | Ag | 50.31% | Acanthite (50.32 %) |
Erythrite | Co3(AsO4)2 · 8H2O | 46.21% | Annabergite (57.77 %) |
Beryl | Be3Al2(Si6O18) | 45.96% | Columbite-(Fe) (57.46 %) |
Skutterudite | CoAs3 | 42.74% | Rammelsbergite (53.43 %) |
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.