Predictive Mineralogy
Possible unrecorded species at Badloch Quarry, Oberbergen, Vogtsburg im Kaiserstuhl, Breisgau-Hochschwarzwald, 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 |
---|---|---|---|
Magnetite | Fe2+Fe3+2O4 | 99.93% | Åkermanite (63.79 %), Andradite (57.68 %), Perovskite (67.07 %), Haüyne (55.34 %), Nepheline (53.00 %), Niocalite (87.50 %), Wöhlerite (50.76 %) |
Quartz | SiO2 | 99.55% | Andradite (57.74 %), Baryte (60.21 %), Calcite (62.43 %), Galena (65.16 %), Niocalite (50.00 %), Wollastonite (59.81 %) |
Pyrite | FeS2 | 98.05% | Baryte (50.79 %), Calcite (51.16 %), Galena (66.84 %), Niocalite (50.00 %), Wollastonite (51.22 %) |
Aegirine | NaFe3+Si2O6 | 89.58% | Niocalite (75.00 %), Wöhlerite (58.33 %) |
Diopside | CaMgSi2O6 | 88.22% | Perovskite (52.40 %), Niocalite (50.00 %), Wollastonite (50.54 %) |
Zircon | Zr(SiO4) | 69.69% | Wöhlerite (69.70 %) |
Sphalerite | ZnS | 66.37% | Galena (65.95 %), Niocalite (50.00 %) |
Chalcopyrite | CuFeS2 | 62.71% | Galena (56.79 %), Niocalite (50.00 %) |
Monticellite | CaMgSiO4 | 62.50% | Niocalite (62.50 %) |
Pyrrhotite | Fe1-xS | 62.50% | Niocalite (62.50 %) |
Natrolite | Na2Al2Si3O10 · 2H2O | 61.36% | Wöhlerite (61.36 %) |
Fluorite | CaF2 | 60.60% | Wöhlerite (60.61 %) |
Analcime | Na(AlSi2O6) · H2O | 59.09% | Wöhlerite (59.09 %) |
Albite | Na(AlSi3O8) | 56.81% | Wöhlerite (56.82 %) |
Microcline | K(AlSi3O8) | 52.27% | Wöhlerite (52.27 %) |
Aegirine-augite | (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6 | 50.00% | Niocalite (50.00 %) |
Alabandite | MnS | 50.00% | Niocalite (50.00 %) |
Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 | 50.00% | Niocalite (50.00 %) |
Fluorapatite | Ca5(PO4)3F | 50.00% | Niocalite (50.00 %) |
Forsterite | Mg2SiO4 | 50.00% | Niocalite (50.00 %) |
Titanite | CaTi(SiO4)O | 50.00% | Niocalite (50.00 %) |
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.