Predictive Mineralogy
Possible unrecorded species at Beauvoir quarry, Échassières, Vichy, Allier, Auvergne-Rhône-Alpes, France
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 | 100.00% | Anglesite (64.19 %), Arsenopyrite (79.40 %), Bariopharmacosiderite (62.90 %), Baryte (50.79 %), Bismite (60.83 %), Bismuth (65.41 %), Cacoxenite (51.90 %), Carminite (64.19 %), Cerussite (56.77 %), Chalcocite (65.95 %), Chalcopyrite (75.16 %), Chalcosiderite (60.47 %), Childrenite (54.63 %), Churchite-(Y) (51.19 %), Corkite (70.95 %), Covellite (80.77 %), Crandallite (50.29 %), Ferberite (59.80 %), Fluorcalciopyrochlore (72.41 %), Galena (66.84 %), Goethite (55.41 %), Goyazite (58.57 %), Hematite (50.17 %), Hemimorphite (54.39 %), Hentschelite (52.17 %), Hinsdalite (66.67 %), Iodargyrite (55.45 %), Jarosite (68.24 %), Kaolinite (52.65 %), Kidwellite (50.00 %), Kintoreite (70.59 %), Lepidocrocite (71.47 %), Libethenite (56.49 %), Marcasite (86.56 %), Mawsonite (79.82 %), Mimetite (59.01 %), Muscovite (50.01 %), Natrojarosite (64.63 %), Parsonsite (51.47 %), Plumbogummite (64.36 %), Pseudomalachite (52.35 %), Pyromorphite (55.98 %), Russellite (55.32 %), Scorodite (67.22 %), Segnitite (74.12 %), Silver (54.72 %), Sphalerite (75.10 %), Stannite (84.48 %), Stolzite (64.97 %), Tsumebite (51.35 %), Uraninite (51.44 %), Varlamoffite (50.79 %), Zavaritskite (62.86 %) |
Malachite | Cu2(CO3)(OH)2 | 99.99% | Anglesite (50.35 %), Bariopharmacosiderite (65.05 %), Carminite (52.56 %), Chalcocite (56.20 %), Chalcosiderite (53.49 %), Chrysocolla (74.38 %), Corkite (63.69 %), Covellite (54.66 %), Hentschelite (78.26 %), Kintoreite (62.75 %), Libethenite (75.09 %), Mimetite (60.02 %), Pseudomalachite (76.53 %), Reichenbachite (86.21 %), Segnitite (59.41 %), Tsumebite (78.38 %) |
Calcite | CaCO3 | 99.99% | Anglesite (53.86 %), Bariopharmacosiderite (52.15 %), Baryte (51.88 %), Cerussite (50.77 %), Corkite (52.51 %), Fluorcalciopyrochlore (82.76 %), Hemimorphite (61.15 %), Jarosite (50.12 %), Lepidocrocite (55.87 %), Marcasite (60.67 %), Mawsonite (50.88 %), Mimetite (56.29 %), Natrojarosite (56.59 %), Tsumebite (64.86 %), Wulfenite (52.13 %) |
Fluorapatite | Ca5(PO4)3F | 99.98% | Brazilianite (55.07 %), Childrenite (62.04 %), Fluorcalciopyrochlore (79.31 %), Hentschelite (52.17 %), Hydroxylherderite (71.97 %), Lacroixite (56.00 %), Montebrasite (58.97 %), Scorzalite (56.34 %), Wardite (64.62 %) |
Microcline | K(AlSi3O8) | 99.75% | Columbite-(Fe) (55.92 %), Columbite-(Mn) (62.20 %), Hydroxylherderite (77.27 %), Lacroixite (52.00 %), Montebrasite (62.82 %), Tantalite-(Mn) (63.90 %) |
Azurite | Cu3(CO3)2(OH)2 | 99.53% | Bariopharmacosiderite (54.30 %), Hentschelite (65.22 %), Libethenite (56.49 %), Pseudomalachite (50.23 %), Reichenbachite (58.62 %), Tsumebite (67.57 %) |
Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 96.99% | Hydroxylherderite (69.70 %), Lacroixite (56.00 %), Montebrasite (54.27 %), Scorzalite (50.70 %) |
Cuprite | Cu2O | 96.96% | Hentschelite (60.87 %), Libethenite (50.53 %), Reichenbachite (58.62 %), Tsumebite (62.16 %) |
Bismuthinite | Bi2S3 | 94.45% | Bismite (60.00 %), Russellite (59.57 %), Zavaritskite (65.71 %) |
Brochantite | Cu4(SO4)(OH)6 | 94.37% | Bariopharmacosiderite (51.61 %), Hentschelite (60.87 %), Tsumebite (70.27 %) |
Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | 85.02% | Parsonsite (69.12 %), Torbernite (51.52 %) |
Pyrrhotite | Fe1-xS | 84.22% | Fluorcalciopyrochlore (55.17 %), Stannite (64.81 %) |
Bornite | Cu5FeS4 | 78.94% | Mawsonite (78.95 %) |
Magnetite | Fe2+Fe3+2O4 | 72.41% | Fluorcalciopyrochlore (72.41 %) |
Aegirine | NaFe3+Si2O6 | 68.96% | Fluorcalciopyrochlore (68.97 %) |
Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 65.11% | Carminite (65.12 %) |
Beraunite | Fe3+6(PO4)4O(OH)4 · 6H2O | 60.00% | Kidwellite (60.00 %) |
Molybdenite | MoS2 | 59.57% | Russellite (59.57 %) |
Spodumene | LiAlSi2O6 | 58.54% | Montebrasite (58.55 %) |
Dufrénite | Ca0.5Fe2+Fe3+5(PO4)4(OH)6 · 2H2O | 58.33% | Kidwellite (58.33 %) |
Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O | 55.88% | Parsonsite (55.88 %) |
Smithsonite | ZnCO3 | 55.58% | Hemimorphite (55.59 %) |
Phlogopite | KMg3(AlSi3O10)(OH)2 | 55.17% | Fluorcalciopyrochlore (55.17 %) |
Rockbridgeite | Fe2+Fe3+4(PO4)3(OH)5 | 55.00% | Kidwellite (55.00 %) |
Linarite | PbCu(SO4)(OH)2 | 54.05% | Tsumebite (54.05 %) |
Chlorargyrite | AgCl | 53.84% | Bromargyrite (53.85 %) |
Stannoidite | Cu+6Cu2+2(Fe2+,Zn)3Sn2S12 | 53.50% | Mawsonite (53.51 %) |
Pyrolusite | Mn4+O2 | 52.33% | Cryptomelane (52.34 %) |
Nepheline | Na3K(Al4Si4O16) | 51.72% | Fluorcalciopyrochlore (51.72 %) |
Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 51.35% | Tsumebite (51.35 %) |
Olivenite | Cu2(AsO4)(OH) | 51.07% | Bariopharmacosiderite (51.08 %) |
Ilmenite | Fe2+TiO3 | 49.65% | Fluorcalciopyrochlore (62.07 %) |
Titanite | CaTi(SiO4)O | 46.89% | Fluorcalciopyrochlore (58.62 %) |
Monazite-(Ce) | Ce(PO4) | 41.37% | Fluorcalciopyrochlore (51.72 %) |
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.