Predictive Mineralogy
Possible unrecorded species at Block 14 opencut, Broken Hill, Broken Hill district, Yancowinna Co., New South Wales, Australia
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% | Adamite (59.33 %), Agardite-(Y) (58.82 %), Anglesite (64.19 %), Arsentsumebite (63.41 %), Atacamite (50.08 %), Aurichalcite (62.90 %), Azurite (58.39 %), Baryte (50.79 %), Bayldonite (57.79 %), Beraunite (54.50 %), Brianyoungite (74.19 %), Brochantite (63.33 %), Calcite (51.16 %), Cerussite (56.77 %), Chalcanthite (74.95 %), Chalcocite (65.95 %), Chalcophanite (56.11 %), Chalcopyrite (75.16 %), Christelite (83.33 %), Conichalcite (51.29 %), Connellite (55.17 %), Corkite (70.95 %), Coronadite (57.93 %), Cuprite (58.26 %), Dufr茅nite (54.49 %), Dyscrasite (72.40 %), Edwardsite (80.00 %), Gahnite (50.30 %), Galena (66.84 %), Goethite (55.41 %), Gordaite (68.18 %), Greenockite (76.91 %), Hemimorphite (54.39 %), Hinsdalite (66.67 %), Hydrozincite (63.58 %), Iodargyrite (55.45 %), Kaolinite (52.65 %), Kintoreite (70.59 %), Kipushite (58.33 %), K枚ttigite (73.91 %), Kr枚hnkite (75.76 %), Ktenasite (75.00 %), Libethenite (56.49 %), Linarite (63.77 %), Malachite (52.79 %), Marshite (75.00 %), Mimetite (59.01 %), Natrojarosite (64.63 %), Niedermayrite (72.73 %), Olivenite (56.33 %), Osakaite (83.33 %), Otavite (70.97 %), Pharmacosiderite (64.43 %), Plimerite (75.00 %), Pseudomalachite (52.35 %), Pyromorphite (55.98 %), Pyrrhotite (80.12 %), Rockbridgeite (52.19 %), Rosasite (63.92 %), Scholzite (52.17 %), Scorodite (67.22 %), Serpierite (71.30 %), Silver (54.72 %), Smithsonite (57.05 %), Sphalerite (75.10 %), Tarbuttite (66.67 %), Tsumebite (51.35 %), Valleriite (77.42 %), Zden臅kite (66.67 %), Zincolivenite (63.41 %) |
| Covellite | CuS | 99.99% | Arsentsumebite (60.98 %), Bayldonite (51.26 %), Christelite (66.67 %), Edwardsite (80.00 %), Gordaite (59.09 %), Kintoreite (60.78 %), Kipushite (50.00 %), Ktenasite (67.39 %), Marshite (68.75 %), Niedermayrite (72.73 %), Osakaite (66.67 %), Plimerite (50.00 %), Serpierite (52.17 %), Tsumebite (51.35 %) |
| Hematite | Fe2O3 | 99.94% | Arsentsumebite (53.66 %), Kipushite (50.00 %), Ktenasite (56.52 %), Marshite (68.75 %), Osakaite (50.00 %), Otavite (51.61 %), Tsumebite (54.05 %), Zden臅kite (66.67 %), Zincolibethenite (50.00 %) |
| Arsenopyrite | FeAsS | 99.72% | Dyscrasite (61.09 %), Edwardsite (80.00 %), Pharmacosiderite (58.74 %), Plimerite (66.67 %), Scorodite (74.10 %) |
| Dolomite | CaMg(CO3)2 | 96.88% | Brianyoungite (52.69 %), Gordaite (54.55 %), K枚ttigite (56.52 %), Zden臅kite (66.67 %) |
| Sulphur | S8 | 95.83% | Edwardsite (80.00 %), Gordaite (50.00 %), Osakaite (58.33 %) |
| Muscovite | KAl2(AlSi3O10)(OH)2 | 95.48% | Gahnite (57.26 %), Kaolinite (51.81 %), Plimerite (50.00 %), Rockbridgeite (56.14 %) |
| Siderite | FeCO3 | 93.33% | Edwardsite (80.00 %), Zden臅kite (66.67 %) |
| Marcasite | FeS2 | 90.90% | Edwardsite (80.00 %), Gordaite (54.55 %) |
| Antlerite | Cu3(SO4)(OH)4 | 90.90% | Edwardsite (80.00 %), Niedermayrite (54.55 %) |
| Jarosite | KFe3+3(SO4)2(OH)6 | 87.50% | Gordaite (50.00 %), Osakaite (50.00 %), Plimerite (50.00 %) |
| Magnetite | Fe2+Fe3+2O4 | 86.56% | Ilmenite (57.89 %), Valleriite (68.10 %) |
| Cacoxenite | Fe3+24AlO6(PO4)17(OH)12 路 75H2O | 84.20% | Beraunite (62.09 %), Plimerite (58.33 %) |
| Ankerite | Ca(Fe2+,Mg)(CO3)2 | 80.00% | Edwardsite (80.00 %) |
| Fluorite | CaF2 | 80.00% | Edwardsite (80.00 %) |
| Hydrocerussite | Pb3(CO3)2(OH)2 | 80.00% | Edwardsite (80.00 %) |
| Duftite | PbCu(AsO4)(OH) | 78.04% | Arsentsumebite (56.10 %), Kipushite (50.00 %) |
| Schulenbergite | (Cu,Zn)7(SO4)2(OH)10 路 3H2O | 75.00% | Osakaite (75.00 %) |
| Cyanotrichite | Cu4Al2(SO4)(OH)12 路 2H2O | 66.66% | Zden臅kite (66.67 %) |
| Plumbogummite | PbAl3(PO4)(PO3OH)(OH)6 | 58.82% | Kintoreite (58.82 %) |
| Langite | Cu4(SO4)(OH)6 路 2H2O | 58.33% | Osakaite (58.33 %) |
| Namuwite | Zn4(SO4)(OH)6 路 4H2O | 58.33% | Osakaite (58.33 %) |
| Posnjakite | Cu4(SO4)(OH)6 路 H2O | 58.33% | Osakaite (58.33 %) |
| Cubanite | CuFe2S3 | 56.27% | Valleriite (56.27 %) |
| Autunite | Ca(UO2)2(PO4)2 路 10-12H2O | 51.51% | Torbernite (51.52 %) |
| Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 51.21% | Arsentsumebite (51.22 %) |
| Theisite | Cu5Zn5(AsO4,SbO4)2(OH)14 | 50.00% | Kipushite (50.00 %) |
| Veszelyite | (Cu,Zn)2Zn(PO4)(OH)3 路 2H2O | 50.00% | Kipushite (50.00 %) |
| Bornite | Cu5FeS4 | 50.00% | Marshite (50.00 %) |
| Ramsbeckite | (Cu,Zn)15(SO4)4(OH)22 路 6H2O | 50.00% | Osakaite (50.00 %) |
| Minohlite | (Cu,Zn)7(SO4)2(OH)10 路 8H2O | 50.00% | Osakaite (50.00 %) |
| Fluorapatite | Ca5(PO4)3F | 50.00% | Plimerite (50.00 %) |
| Wulfenite | Pb(MoO4) | 43.24% | Tsumebite (54.05 %) |
| Gold | Au | 40.00% | Marshite (50.00 %) |
| Molybdenite | MoS2 | 40.00% | Marshite (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.