Predictive Mineralogy
Possible unrecorded species at Gerstenegg-Sommerloch tunnel, Gerstenegg, Guttannen, Interlaken-Oberhasli, Bern, Switzerland
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 | 89.55% | Bayleyite (54.55 %), Monazite-(Ce) (77.02 %) |
| Calcite | CaCO3 | 88.24% | Bayleyite (61.36 %), Monohydrocalcite (69.57 %) |
| Uraninite | UO2 | 82.20% | Bayleyite (59.09 %), Schröckingerite (56.49 %) |
| Gypsum | CaSO4 · 2H2O | 82.08% | Bayleyite (61.36 %), Monohydrocalcite (53.62 %) |
| Pyrite | FeS2 | 65.90% | Bayleyite (65.91 %) |
| Albite | Na(AlSi3O8) | 51.77% | Monazite-(Ce) (51.78 %) |
| Muscovite | KAl2(AlSi3O10)(OH)2 | 51.25% | Monazite-(Ce) (51.26 %) |
| Zircon | Zr(SiO4) | 43.98% | Monazite-(Ce) (54.99 %) |
| Chalcopyrite | CuFeS2 | 40.00% | Bayleyite (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.