Predictive Mineralogy
Possible unrecorded species at Lower Schindelmatt adit (Gespreng veins), 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 |
---|---|---|---|
Galena | PbS | 99.16% | Descloizite (66.30 %), Pyromorphite (77.81 %), Vanadinite (63.81 %), Wulfenite (69.21 %) |
Quartz | SiO2 | 98.20% | Descloizite (60.18 %), Pyromorphite (69.73 %), Vanadinite (58.84 %), Wulfenite (63.76 %) |
Cerussite | PbCO3 | 97.62% | Descloizite (60.18 %), Pyromorphite (68.61 %), Vanadinite (54.01 %), Wulfenite (58.77 %) |
Calcite | CaCO3 | 89.84% | Descloizite (55.36 %), Vanadinite (52.49 %), Wulfenite (52.13 %) |
Malachite | Cu2(CO3)(OH)2 | 83.87% | Cornetite (83.87 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 ยท nH2O, x < 1 | 70.96% | Cornetite (70.97 %) |
Pseudomalachite | Cu5(PO4)2(OH)4 | 64.51% | Cornetite (64.52 %) |
Sphalerite | ZnS | 56.90% | Pyromorphite (56.90 %) |
Pyrite | FeS2 | 55.98% | Pyromorphite (55.98 %) |
Chalcopyrite | CuFeS2 | 54.90% | Pyromorphite (54.91 %) |
Brochantite | Cu4(SO4)(OH)6 | 54.83% | Cornetite (54.84 %) |
Azurite | Cu3(CO3)2(OH)2 | 51.61% | Cornetite (51.61 %) |
Libethenite | Cu2(PO4)(OH) | 51.61% | Cornetite (51.61 %) |
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.