Predictive Mineralogy
Possible unrecorded species at Roua Mines (Clue de Roua), Daluis, Nice, Alpes-Maritimes, Provence-Alpes-Côte d'Azur, 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 |
---|---|---|---|
Chalcopyrite | CuFeS2 | 100.00% | Acanthite (62.06 %), Adamite (60.33 %), Ankerite (62.42 %), Atacamite (53.76 %), Aurichalcite (64.77 %), Azurite (65.18 %), Brochantite (71.06 %), Caledonite (65.04 %), Chalcophyllite (75.56 %), Chrysocolla (56.02 %), Claringbullite (70.59 %), Conichalcite (53.65 %), Connellite (65.52 %), Copper (53.15 %), Cornubite (62.31 %), Covellite (85.83 %), Cuprite (67.05 %), Djurleite (72.46 %), Gerhardtite (57.14 %), Gilmarite (70.00 %), Koutekite (57.14 %), Langite (78.16 %), Malachite (60.66 %), Mixite (63.02 %), Olivenite (65.16 %), Parnauite (77.60 %), Pharmacosiderite (59.35 %), Posnjakite (77.25 %), Rouaite (56.25 %), Siderite (51.43 %), Silver (50.22 %), Tangdanite (66.67 %), Tenorite (68.61 %), Trippkeite (50.00 %), Tyrolite (66.20 %), Vésigniéite (50.00 %), Wallkilldellite (54.55 %) |
Pyrite | FeS2 | 99.99% | Acanthite (68.82 %), Adamite (59.33 %), Ankerite (75.64 %), Atacamite (50.08 %), Aurichalcite (62.90 %), Azurite (58.39 %), Baryte (50.79 %), Brochantite (63.33 %), Calcite (51.16 %), Caledonite (59.41 %), Chalcophyllite (65.78 %), Claringbullite (64.71 %), Conichalcite (51.29 %), Connellite (55.17 %), Cornubite (50.00 %), Covellite (80.77 %), Cuprite (58.26 %), Djurleite (66.09 %), Dolomite (58.22 %), Gerhardtite (53.57 %), Gilmarite (60.00 %), Goethite (55.41 %), Kolfanite (57.14 %), Koutekite (52.38 %), Langite (68.50 %), Malachite (52.79 %), Mixite (52.60 %), Olivenite (56.33 %), Parnauite (64.80 %), Pharmacosiderite (64.43 %), Posnjakite (70.22 %), Siderite (66.11 %), Silver (54.72 %), Tenorite (59.82 %), Trippkeite (62.50 %), Tyrolite (57.84 %), Vésigniéite (53.85 %) |
Galena | PbS | 99.99% | Acanthite (69.24 %), Adamite (66.33 %), Ankerite (54.09 %), Aurichalcite (74.95 %), Brochantite (55.97 %), Caledonite (82.40 %), Chalcophyllite (55.56 %), Chlorargyrite (55.61 %), Covellite (64.18 %), Djurleite (51.01 %), Langite (63.00 %), Olivenite (50.95 %), Parnauite (60.80 %), Pharmacosiderite (51.63 %), Posnjakite (59.83 %), Silver (52.62 %) |
Sphalerite | ZnS | 99.99% | Acanthite (62.85 %), Adamite (55.00 %), Ankerite (53.36 %), Aurichalcite (70.37 %), Brochantite (50.32 %), Caledonite (62.35 %), Chalcophyllite (54.67 %), Covellite (64.68 %), Langite (58.40 %), Parnauite (50.40 %), Posnjakite (55.90 %), Trippkeite (50.00 %) |
Chalcocite | Cu2S | 99.94% | Algodonite (50.00 %), Claringbullite (52.94 %), Covellite (50.30 %), Djurleite (62.90 %), Domeykite (54.32 %), Gilmarite (60.00 %), Koutekite (66.67 %), Rouaite (56.25 %), Tenorite (51.44 %) |
Cerussite | PbCO3 | 99.90% | Adamite (60.00 %), Aurichalcite (64.77 %), Caledonite (85.33 %), Claringbullite (58.82 %), Langite (53.94 %), Parnauite (51.20 %), Posnjakite (50.00 %) |
Hematite | Fe2O3 | 97.77% | Djurleite (51.01 %), Gilmarite (60.00 %), Trippkeite (50.00 %), Wallkilldellite (77.27 %) |
Bornite | Cu5FeS4 | 91.44% | Djurleite (64.06 %), Koutekite (52.38 %), Rouaite (50.00 %) |
Gypsum | CaSO4 · 2H2O | 91.44% | Claringbullite (52.94 %), Posnjakite (58.43 %), Rouaite (56.25 %) |
Anglesite | PbSO4 | 88.14% | Caledonite (76.28 %), Trippkeite (50.00 %) |
Arsenopyrite | FeAsS | 84.52% | Pharmacosiderite (58.74 %), Trippkeite (62.50 %) |
Cornwallite | Cu5(AsO4)2(OH)4 | 83.07% | Cornubite (57.69 %), Gilmarite (60.00 %) |
Linarite | PbCu(SO4)(OH)2 | 81.17% | Caledonite (81.17 %) |
Mimetite | Pb5(AsO4)3Cl | 79.82% | Adamite (58.67 %), Parnauite (51.20 %) |
Hemimorphite | Zn4Si2O7(OH)2 · H2O | 76.69% | Aurichalcite (50.47 %), Claringbullite (52.94 %) |
Hollandite | Ba(Mn4+6Mn3+2)O16 | 66.66% | Janggunite (66.67 %) |
Scorodite | Fe3+AsO4 · 2H2O | 61.99% | Pharmacosiderite (61.99 %) |
Aegirine | NaFe3+Si2O6 | 59.09% | Wallkilldellite (59.09 %) |
Rhodonite | CaMn3Mn[Si5O15] | 59.09% | Wallkilldellite (59.09 %) |
Bismuthinite | Bi2S3 | 57.14% | Kolfanite (57.14 %) |
Bismuth | Bi | 57.14% | Wallkilldellite-(Fe) (57.14 %) |
Smithsonite | ZnCO3 | 54.57% | Aurichalcite (54.58 %) |
Braunite | Mn2+Mn3+6(SiO4)O8 | 54.54% | Wallkilldellite (54.55 %) |
Volborthite | Cu3(V2O7)(OH)2 · 2H2O | 53.84% | Vésigniéite (53.85 %) |
Paratacamite | Cu3(Cu,Zn)(OH)6Cl2 | 52.94% | Claringbullite (52.94 %) |
Spangolite | Cu6Al(SO4)(OH)12Cl · 3H2O | 52.94% | Claringbullite (52.94 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 52.79% | Albite (52.80 %) |
Magnetite | Fe2+Fe3+2O4 | 52.17% | Pecoraite (52.17 %) |
Kutnohorite | CaMn2+(CO3)2 | 50.00% | Wallkilldellite (50.00 %) |
Manganberzeliite | (NaCa2)Mn2+2(AsO4)3 | 50.00% | Wallkilldellite (50.00 %) |
Rhodochrosite | MnCO3 | 50.00% | Wallkilldellite (50.00 %) |
Arseniosiderite | Ca2Fe3+3(AsO4)3O2 · 3H2O | 50.00% | Gilmarite (50.00 %) |
Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 50.00% | Gilmarite (50.00 %) |
Rutile | TiO2 | 40.00% | Trippkeite (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.