Predictive Mineralogy
Possible unrecorded species at Wieden, Lörrach, Freiburg Region, Baden-Württemberg, Germany
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 |
|---|---|---|---|
| Arsenopyrite | FeAsS | 99.14% | Argentopyrite (50.75 %), Arsenic (53.29 %), Arsenolite (55.13 %), Carminite (53.49 %), Miargyrite (53.57 %), Schultenite (61.54 %) |
| Acanthite | Ag2S | 98.60% | Argentopyrite (62.69 %), Miargyrite (53.30 %), Proustite (55.52 %), Schultenite (56.41 %), Stephanite (58.82 %) |
| Pyrargyrite | Ag3SbS3 | 97.63% | Argentopyrite (59.70 %), Miargyrite (70.05 %), Proustite (53.45 %), Stephanite (57.94 %) |
| Scorodite | Fe3+AsO4 · 2H2O | 93.73% | Arsenbrackebuschite (50.00 %), Carminite (65.12 %), Schultenite (64.10 %) |
| Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 92.98% | Arsenbrackebuschite (53.85 %), Carminite (65.12 %), Schultenite (56.41 %) |
| Smithsonite | ZnCO3 | 91.58% | Arsenbrackebuschite (50.00 %), Hemimorphite (55.59 %), Hydrozincite (62.08 %) |
| Cuprite | Cu2O | 79.86% | Arsenbrackebuschite (50.00 %), Langite (59.73 %) |
| Uraninite | UO2 | 76.95% | Metazeunerite (53.70 %), Zeunerite (50.23 %) |
| Linarite | PbCu(SO4)(OH)2 | 62.67% | Leadhillite (62.67 %) |
| Albite | Na(AlSi3O8) | 59.32% | Bastnäsite-(Ce) (59.33 %) |
| Magnetite | Fe2+Fe3+2O4 | 58.80% | Bastnäsite-(Ce) (58.81 %) |
| Adamite | Zn2(AsO4)(OH) | 53.84% | Arsenbrackebuschite (53.85 %) |
| Hematite | Fe2O3 | 53.84% | Arsenbrackebuschite (53.85 %) |
| Jarosite | KFe3+3(SO4)2(OH)6 | 53.84% | Arsenbrackebuschite (53.85 %) |
| Zircon | Zr(SiO4) | 52.84% | Bastnäsite-(Ce) (66.06 %) |
| Microcline | K(AlSi3O8) | 50.77% | Bastnäsite-(Ce) (50.78 %) |
| Copper | Cu | 50.00% | Arsenbrackebuschite (50.00 %) |
| Duftite | PbCu(AsO4)(OH) | 50.00% | Arsenbrackebuschite (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.