Predictive Mineralogy
Possible unrecorded species at U obr谩zku quarry (Obr谩zek I quarry), P铆sek District, South Bohemian Region, Czech Republic
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 |
---|---|---|---|
Calcite | CaCO3 | 99.97% | Chondrodite (65.81 %), Delvauxite (70.83 %), Jarosite (50.12 %), Kahlerite (64.71 %), Natrojarosite (56.59 %), Phlogopite (55.90 %), Pitticite (65.33 %), Symplesite (52.43 %), Titanite (52.17 %) |
Scorodite | Fe3+AsO4 路 2H2O | 93.08% | Pharmacosiderite (61.99 %), Pitticite (50.67 %), Symplesite (63.11 %) |
Gypsum | CaSO4 路 2H2O | 92.95% | Delvauxite (52.08 %), Kahlerite (58.82 %), Natrojarosite (64.31 %) |
Malachite | Cu2(CO3)(OH)2 | 81.60% | Kahlerite (58.82 %), Pitticite (55.33 %) |
Galena | PbS | 78.56% | Arsenopyrite (53.61 %), Chalcopyrite (51.07 %), Pharmacosiderite (51.63 %), Pitticite (62.67 %), Symplesite (56.31 %) |
Zircon | Zr(SiO4) | 77.79% | Fergusonite-(Y) (69.95 %), Foitite (52.75 %), Monazite-(Ce) (54.99 %), Xenotime-(Y) (56.84 %) |
Sphalerite | ZnS | 77.31% | Arsenopyrite (55.02 %), Chalcopyrite (50.66 %), Pitticite (60.00 %), Symplesite (62.14 %) |
Uraninite | UO2 | 70.58% | Kahlerite (70.59 %) |
Covellite | CuS | 58.82% | Kahlerite (58.82 %) |
Schoepite | (UO2)8O2(OH)12 路 12H2O | 58.82% | Kahlerite (58.82 %) |
Diopside | CaMgSi2O6 | 54.63% | Chondrodite (54.63 %) |
Goethite | 伪-Fe3+O(OH) | 54.16% | Delvauxite (54.17 %) |
Columbite-(Mn) | Mn2+Nb2O6 | 53.65% | Rossmanite (53.66 %) |
Meta-autunite | Ca(UO2)2(PO4)2 路 6H2O | 52.94% | Kahlerite (52.94 %) |
Uranophane | Ca(UO2)2(SiO3OH)2 路 5H2O | 52.94% | Kahlerite (52.94 %) |
Zeunerite | Cu(UO2)2(AsO4)2 路 12H2O | 52.94% | Kahlerite (52.94 %) |
Fluorapatite | Ca5(PO4)3F | 52.74% | Foitite (52.75 %) |
Baryte | BaSO4 | 51.76% | Kahlerite (64.71 %) |
Autunite | Ca(UO2)2(PO4)2 路 10-12H2O | 51.51% | Torbernite (51.52 %) |
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.