Predictive Mineralogy
Possible unrecorded species at Barbara vein, Hofsgrund (South field), Hofsgrund, Oberried, Breisgau-Hochschwarzwald, Freiburg Region, Baden-Wรผrttemberg, 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 |
|---|---|---|---|
| Quartz | SiO2 | 99.99% | Acanthite (72.42 %), Beudantite (75.51 %), Brochantite (70.20 %), Caledonite (75.06 %), Carminite (77.21 %), Chrysocolla (61.53 %), Descloizite (60.18 %), Erythrite (69.80 %), Galena (65.16 %), Hemimorphite (61.55 %), Leadhillite (74.32 %), Linarite (74.40 %), Malachite (61.21 %), Pyromorphite (69.73 %), Silver (59.03 %), Wulfenite (63.76 %) |
| Chalcopyrite | CuFeS2 | 99.99% | Acanthite (62.06 %), Beudantite (61.52 %), Brochantite (71.06 %), Caledonite (65.04 %), Carminite (60.93 %), Chrysocolla (56.02 %), Erythrite (69.91 %), Galena (56.79 %), Leadhillite (57.88 %), Linarite (69.97 %), Malachite (60.66 %), Pyromorphite (54.91 %), Silver (50.22 %) |
| Pyrite | FeS2 | 99.99% | Acanthite (68.82 %), Beudantite (62.96 %), Brochantite (63.33 %), Caledonite (59.41 %), Carminite (64.19 %), Erythrite (64.88 %), Galena (66.84 %), Hemimorphite (54.39 %), Leadhillite (56.51 %), Linarite (63.77 %), Malachite (52.79 %), Pyromorphite (55.98 %), Silver (54.72 %) |
| Cerussite | PbCO3 | 99.99% | Beudantite (65.23 %), Caledonite (85.33 %), Carminite (58.60 %), Descloizite (60.18 %), Hemimorphite (64.31 %), Leadhillite (88.70 %), Linarite (77.95 %), Pyromorphite (68.61 %), Wulfenite (58.77 %) |
| Sphalerite | ZnS | 99.99% | Acanthite (62.85 %), Beudantite (60.29 %), Brochantite (50.32 %), Caledonite (62.35 %), Carminite (55.81 %), Erythrite (50.44 %), Galena (65.95 %), Hemimorphite (68.27 %), Leadhillite (58.56 %), Linarite (66.52 %), Pyromorphite (56.90 %) |
| Calcite | CaCO3 | 99.94% | Acanthite (51.71 %), Brochantite (53.68 %), Caledonite (54.52 %), Descloizite (55.36 %), Erythrite (59.85 %), Hemimorphite (61.15 %), Leadhillite (63.36 %), Linarite (56.51 %), Wulfenite (52.13 %) |
| Anglesite | PbSO4 | 99.60% | Beudantite (54.12 %), Caledonite (76.28 %), Carminite (53.02 %), Leadhillite (78.77 %), Linarite (63.68 %) |
| Goethite | ฮฑ-Fe3+O(OH) | 90.75% | Beudantite (54.12 %), Carminite (57.67 %), Leadhillite (52.40 %) |
| Mimetite | Pb5(AsO4)3Cl | 85.68% | Beudantite (54.73 %), Carminite (68.37 %) |
| Scorodite | Fe3+AsO4 ยท 2H2O | 65.11% | Carminite (65.12 %) |
| Pseudomalachite | Cu5(PO4)2(OH)4 | 64.51% | Cornetite (64.52 %) |
| Smithsonite | ZnCO3 | 55.58% | Hemimorphite (55.59 %) |
| Arsenopyrite | FeAsS | 53.48% | Carminite (53.49 %) |
| Azurite | Cu3(CO3)2(OH)2 | 51.61% | Cornetite (51.61 %) |
| Libethenite | Cu2(PO4)(OH) | 51.61% | Cornetite (51.61 %) |
| Covellite | CuS | 50.12% | Caledonite (50.12 %) |
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.