Predictive Mineralogy
Possible unrecorded species at Mont-des-Groseillers, Blaton, Bernissart, Hainaut, Wallonia, Belgium
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 |
---|---|---|---|
Chalcopyrite | CuFeS2 | 99.90% | Allophane (55.04 %), Ferroberaunite (53.85 %), Jarosite (50.73 %), Lepidocrocite (58.40 %), Malachite (60.66 %), Melanterite (53.65 %), Pyrite (51.72 %), Rozenite (50.30 %), Siderite (51.43 %) |
Fluorapatite | Ca5(PO4)3F | 99.35% | Ferroberaunite (65.38 %), Mitridatite (62.25 %), Phosphosiderite (50.71 %), Strunzite (64.76 %), Whitmoreite (71.43 %) |
Albite | Na(AlSi3O8) | 98.29% | Ferroberaunite (50.00 %), Mitridatite (54.30 %), Strunzite (68.57 %), Whitmoreite (76.19 %) |
Goethite | Ξ±-Fe3+O(OH) | 95.83% | Delvauxite (54.17 %), Ferroberaunite (61.54 %), Lepidocrocite (76.37 %) |
Microcline | K(AlSi3O8) | 90.13% | Mitridatite (51.66 %), Strunzite (57.14 %), Whitmoreite (52.38 %) |
Hematite | Fe2O3 | 79.28% | Ferroberaunite (53.85 %), Lepidocrocite (55.13 %) |
Sphalerite | ZnS | 77.24% | Diadochite (57.83 %), Ferroberaunite (61.54 %), Melanterite (50.38 %), Whitmoreite (57.14 %) |
Beryl | Be3Al2(Si6O18) | 74.64% | Mitridatite (54.30 %), Strunzite (67.62 %), Whitmoreite (54.76 %) |
Triphylite | LiFe2+PO4 | 70.85% | Strunzite (60.00 %), Whitmoreite (71.43 %) |
Zircon | Zr(SiO4) | 66.93% | Strunzite (54.29 %), Whitmoreite (64.29 %) |
Arsenopyrite | FeAsS | 65.49% | Ferroberaunite (57.69 %), Whitmoreite (57.14 %) |
Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 65.48% | Strunzite (52.38 %), Whitmoreite (61.90 %) |
Heterosite | (Fe3+,Mn3+)PO4 | 61.90% | Whitmoreite (61.90 %) |
Sulphur | S8 | 60.63% | Metavoltine (60.64 %) |
Laueite | Mn2+Fe3+2(PO4)2(OH)2 Β· 8H2O | 52.38% | Whitmoreite (52.38 %) |
Almandine | Fe2+3Al2(SiO4)3 | 50.00% | Whitmoreite (50.00 %) |
Autunite | Ca(UO2)2(PO4)2 Β· 10-12H2O | 49.52% | Whitmoreite (61.90 %) |
Torbernite | Cu(UO2)2(PO4)2 Β· 12H2O | 40.00% | Ferroberaunite (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.