Predictive Mineralogy
Possible unrecorded species at Weckersdorf quarry, Zeulenroda-Triebes, Greiz District, Thuringia, 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 |
---|---|---|---|
Pyrite | FeS2 | 99.50% | Allophane (60.97 %), Baryte (50.79 %), Goethite (55.41 %), Hematite (50.17 %), Jarosite (68.24 %), Tinticite (63.64 %) |
Calcite | CaCO3 | 95.64% | Allophane (61.15 %), Baryte (51.88 %), Jarosite (50.12 %), Kingite (53.33 %) |
Chalcopyrite | CuFeS2 | 77.84% | Allophane (55.04 %), Jarosite (50.73 %) |
Cacoxenite | Fe3+24AlO6(PO4)17(OH)12 Β· 75H2O | 76.66% | Kingite (53.33 %), Tinticite (50.00 %) |
Strengite | FePO4 Β· 2H2O | 54.54% | Tinticite (54.55 %) |
Wavellite | Al3(PO4)2(OH,F)3 Β· 5H2O | 53.33% | Kingite (53.33 %) |
Malachite | Cu2(CO3)(OH)2 | 53.23% | Allophane (53.24 %) |
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.