Predictive Mineralogy
Possible unrecorded species at Cerro Moreno volcano (Cerro Moreno quarry), Almagro, 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 |
---|---|---|---|
Analcime | Na(AlSi2O6) · H2O | 98.99% | Gonnardite (67.86 %), Lévyne-Ca (64.00 %), Natrolite (56.38 %), Phillipsite-Ca (53.33 %), Thomsonite-Ca (57.41 %) |
Quartz | SiO2 | 98.21% | Baryte (60.21 %), Calcite (62.43 %), Chabazite-Ca (50.66 %), Hydrotalcite (50.00 %), Thaumasite (51.69 %) |
Pyrite | FeS2 | 94.41% | Baryte (50.79 %), Calcite (51.16 %), Hydrotalcite (51.89 %), Thaumasite (51.69 %) |
Magnetite | Fe2+Fe3+2O4 | 91.54% | Hydrotalcite (60.38 %), Nepheline (53.00 %), Thaumasite (54.59 %) |
Aragonite | CaCO3 | 55.66% | Hydrotalcite (55.66 %) |
Brucite | Mg(OH)2 | 50.94% | Hydrotalcite (50.94 %) |
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.