Predictive Mineralogy
Possible unrecorded species at Silver mine, Zimmerbach, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France
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 |
|---|---|---|---|
| Galena | PbS | 99.99% | Acanthite (69.24 %), Ankerite (54.09 %), Arseniosiderite (52.21 %), Bariopharmacosiderite (53.23 %), Bayldonite (74.37 %), Beaverite-(Cu) (82.63 %), Beudantite (76.34 %), Brochantite (55.97 %), Carminite (71.16 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Digenite (59.98 %), Olivenite (50.95 %) |
| Calcite | CaCO3 | 99.99% | Acanthite (51.71 %), Allophane (61.15 %), Ankerite (66.26 %), Arseniosiderite (65.04 %), Bariopharmacosiderite (52.15 %), Baryte (51.88 %), Beaverite-(Cu) (58.08 %), Brochantite (53.68 %), Cornubite (50.77 %), Cornwallite (50.24 %), Digenite (52.28 %), Jarosite (50.12 %), Mixite (51.56 %), Olivenite (50.43 %), Siderite (52.18 %), Zálesíite (68.32 %) |
| Cerussite | PbCO3 | 98.96% | Bayldonite (73.37 %), Beaverite-(Cu) (73.05 %), Beudantite (65.23 %), Carminite (58.60 %) |
| Anglesite | PbSO4 | 96.61% | Bayldonite (52.26 %), Beaverite-(Cu) (67.07 %), Beudantite (54.12 %), Carminite (53.02 %) |
| Scorodite | Fe3+AsO4 · 2H2O | 85.18% | Arseniosiderite (57.52 %), Carminite (65.12 %) |
| Gypsum | CaSO4 · 2H2O | 80.88% | Anhydrite (61.07 %), Beaverite-(Cu) (50.90 %) |
| Sphalerite | ZnS | 79.98% | Acanthite (62.85 %), Ankerite (53.36 %), Bayldonite (55.28 %), Beaverite-(Cu) (66.47 %), Beudantite (60.29 %), Brochantite (50.32 %), Carminite (55.81 %), Chalcopyrite (50.66 %), Covellite (64.68 %), Digenite (61.34 %) |
| Mimetite | Pb5(AsO4)3Cl | 76.77% | Bayldonite (71.86 %), Beudantite (54.73 %), Carminite (68.37 %) |
| Arsenopyrite | FeAsS | 53.48% | Carminite (53.49 %) |
| Linarite | PbCu(SO4)(OH)2 | 52.09% | Beaverite-(Cu) (52.10 %) |
| Silver | Ag | 50.31% | Acanthite (50.32 %) |
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.