Predictive Mineralogy
Possible unrecorded species at La Estrella mine (La Platilla mine), Pardos deposit, Pardos, Guadalajara, 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 |
---|---|---|---|
Calcite | CaCO3 | 99.99% | Anglesite (53.86 %), Arseniosiderite (65.04 %), Arsentsumebite (65.85 %), Bariopharmacosiderite (52.15 %), Baryte (51.88 %), Beaverite-(Cu) (58.08 %), Cerussite (50.77 %), Cornwallite (50.24 %), Duftite (57.87 %), Hidalgoite (54.55 %), Mimetite (56.29 %), Olivenite (50.43 %), Oxyplumboroméite (56.16 %), Tripuhyite (60.71 %) |
Brochantite | Cu4(SO4)(OH)6 | 99.74% | Arsentsumebite (63.41 %), Bariopharmacosiderite (51.61 %), Bayldonite (57.29 %), Beaverite-(Cu) (67.66 %), Clinoclase (55.48 %), Cornwallite (52.15 %), Hidalgoite (50.65 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 | 96.53% | Arsentsumebite (68.29 %), Clinoclase (52.74 %), Cornwallite (52.63 %), Duftite (51.18 %) |
Scorodite | Fe3+AsO4 · 2H2O | 92.68% | Arseniosiderite (57.52 %), Carminite (65.12 %), Hidalgoite (50.65 %) |
Gypsum | CaSO4 · 2H2O | 92.37% | Arsentsumebite (65.85 %), Beaverite-(Cu) (50.90 %), Hidalgoite (54.55 %) |
Covellite | CuS | 90.88% | Arsentsumebite (60.98 %), Bayldonite (51.26 %), Beaverite-(Cu) (52.10 %) |
Hematite | Fe2O3 | 90.72% | Arsentsumebite (53.66 %), Hidalgoite (54.55 %), Tripuhyite (55.95 %) |
Linarite | PbCu(SO4)(OH)2 | 80.13% | Arsentsumebite (58.54 %), Beaverite-(Cu) (52.10 %) |
Arsenopyrite | FeAsS | 80.02% | Carminite (53.49 %), Segnitite (57.06 %) |
Sphalerite | ZnS | 79.99% | Anglesite (64.09 %), Arsentsumebite (60.98 %), Bayldonite (55.28 %), Beaverite-(Cu) (66.47 %), Beudantite (60.29 %), Carminite (55.81 %), Cerussite (56.70 %), Chalcopyrite (50.66 %), Duftite (51.18 %), Galena (65.95 %), Hidalgoite (61.04 %), Mimetite (53.11 %), Oxyplumboroméite (65.75 %), Segnitite (67.06 %) |
Pseudomalachite | Cu5(PO4)2(OH)4 | 59.29% | Libethenite (59.30 %) |
Jarosite | KFe3+3(SO4)2(OH)6 | 55.84% | Hidalgoite (55.84 %) |
Stibnite | Sb2S3 | 53.57% | Tripuhyite (53.57 %) |
Chalcocite | Cu2S | 51.43% | Tenorite (51.44 %) |
Smithsonite | ZnCO3 | 44.87% | Arsentsumebite (56.10 %) |
Hemimorphite | Zn4Si2O7(OH)2 · H2O | 42.92% | Arsentsumebite (53.66 %) |
Gold | Au | 40.00% | Tripuhyite (50.00 %) |
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.