Predictive Mineralogy
Possible unrecorded species at Clara adit (dump), Wittichen, Schenkenzell, Rottweil, 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 |
---|---|---|---|
Quartz | SiO2 | 90.68% | Agardite-(Nd) (78.95 %), Uranospinite (55.74 %) |
Chalcopyrite | CuFeS2 | 87.48% | Agardite-(Nd) (73.68 %), Uranospinite (52.46 %) |
Calcite | CaCO3 | 87.05% | Agardite-(Nd) (68.42 %), Uranospinite (59.02 %) |
Pyrite | FeS2 | 87.05% | Agardite-(Nd) (68.42 %), Uranospinite (59.02 %) |
Malachite | Cu2(CO3)(OH)2 | 78.94% | Agardite-(Nd) (78.95 %) |
Uraninite | UO2 | 73.77% | Uranospinite (73.77 %) |
Cuprite | Cu2O | 68.42% | Agardite-(Nd) (68.42 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 | 63.15% | Agardite-(Nd) (63.16 %) |
Galena | PbS | 58.94% | Agardite-(Nd) (73.68 %) |
Azurite | Cu3(CO3)2(OH)2 | 57.89% | Agardite-(Nd) (57.89 %) |
Hematite | Fe2O3 | 57.89% | Agardite-(Nd) (57.89 %) |
Brochantite | Cu4(SO4)(OH)6 | 52.63% | Agardite-(Nd) (52.63 %) |
Chalcocite | Cu2S | 52.63% | Agardite-(Nd) (52.63 %) |
Conichalcite | CaCu(AsO4)(OH) | 52.63% | Agardite-(Nd) (52.63 %) |
Copper | Cu | 52.63% | Agardite-(Nd) (52.63 %) |
Dolomite | CaMg(CO3)2 | 52.63% | Agardite-(Nd) (52.63 %) |
Olivenite | Cu2(AsO4)(OH) | 52.63% | Agardite-(Nd) (52.63 %) |
Baryte | BaSO4 | 46.31% | Agardite-(Nd) (57.89 %) |
Cerussite | PbCO3 | 46.31% | Agardite-(Nd) (57.89 %) |
Mimetite | Pb5(AsO4)3Cl | 46.31% | Agardite-(Nd) (57.89 %) |
Mixite | BiCu6(AsO4)3(OH)6 · 3H2O | 46.31% | Agardite-(Nd) (57.89 %) |
Silver | Ag | 46.31% | Agardite-(Nd) (57.89 %) |
Sphalerite | ZnS | 46.31% | Agardite-(Nd) (57.89 %) |
Agardite-(Y) | YCu6(AsO4)3(OH)6 · 3H2O | 42.10% | Agardite-(Nd) (52.63 %) |
Agardite-(Ce) | CeCu6(AsO4)3(OH)6 · 3H2O | 42.10% | Agardite-(Nd) (52.63 %) |
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.