Predictive Mineralogy
Possible unrecorded species at Campo de Calatrava volcanic field, Ciudad Real, Castile-La Mancha, Spain
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% | Aragonite (53.70 %), Baryte (60.21 %), Birnessite (58.41 %), Calcite (62.43 %), Chabazite-Ca (50.66 %), Copper (56.56 %), Cryptomelane (56.26 %), Diopside (51.68 %), Hydrotalcite (50.00 %), Hydroxyapophyllite-(K) (57.29 %), Hydroxylapatite (58.93 %), Lithiophorite (53.91 %), Magnetite (50.54 %), Opal (60.07 %), Thaumasite (51.69 %), Todorokite (70.08 %) |
Analcime | Na(AlSi2O6) · H2O | 99.51% | Gonnardite (67.86 %), Lévyne-Ca (64.00 %), Natrolite (56.38 %), Phillipsite-Ca (53.33 %), Phillipsite-K (51.58 %), Thomsonite-Ca (57.41 %) |
Pyrite | FeS2 | 97.49% | Baryte (50.79 %), Calcite (51.16 %), Hydrotalcite (51.89 %), Hydroxyapophyllite-(K) (55.21 %), Thaumasite (51.69 %) |
Gypsum | CaSO4 · 2H2O | 58.03% | Ettringite (58.04 %) |
Chalcopyrite | CuFeS2 | 53.15% | Copper (53.15 %) |
Pyrolusite | Mn4+O2 | 52.33% | Cryptomelane (52.34 %) |
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.