Predictive Mineralogy
Possible unrecorded species at Apollo Mine, Raubach, Puderbach, Neuwied, Rhineland-Palatinate, 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 | 99.99% | Berthierite (68.55 %), Boulangerite (64.45 %), Bournonite (55.79 %), Jamesonite (63.81 %), Jask贸lskiite (86.67 %), Meneghinite (69.40 %), Metastibnite (53.00 %), Plagionite (69.03 %), Semseyite (59.91 %), Senarmontite (52.66 %), Zinkenite (59.48 %) |
Marcasite | FeS2 | 92.84% | Jask贸lskiite (66.67 %), Plagionite (56.64 %), Semseyite (50.47 %) |
Gypsum | CaSO4 路 2H2O | 91.28% | Beaverite-(Cu) (50.90 %), Natrojarosite (64.31 %), Sulphur (50.28 %) |
Pyrrhotite | Fe1-xS | 89.50% | Jask贸lskiite (73.33 %), Meneghinite (60.66 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 78.74% | Jask贸lskiite (53.33 %), Tetrahedrite-(Zn) (54.46 %) |
Pyrolusite | Mn4+O2 | 63.98% | Manganite (63.98 %) |
Hemimorphite | Zn4Si2O7(OH)2 路 H2O | 63.73% | Rosasite (63.74 %) |
Baryte | BaSO4 | 62.19% | Beaverite-(Cu) (55.09 %), Plagionite (50.44 %) |
Magnetite | Fe2+Fe3+2O4 | 60.00% | Jask贸lskiite (60.00 %) |
Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 59.34% | Rosasite (59.34 %) |
Smithsonite | ZnCO3 | 57.69% | Rosasite (57.69 %) |
Albite | Na(AlSi3O8) | 53.33% | Jask贸lskiite (53.33 %) |
Kaolinite | Al2(Si2O5)(OH)4 | 50.40% | Dickite (50.40 %) |
Silver | Ag | 50.31% | Acanthite (50.32 %) |
Chalcocite | Cu2S | 50.30% | Covellite (50.30 %) |
Bismuth | Bi | 48.00% | Jask贸lskiite (60.00 %) |
Gold | Au | 42.66% | Jask贸lskiite (53.33 %) |
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.