Predictive Mineralogy
Possible unrecorded species at Beyrède-Jumet, Aure Valley, Hautes-Pyrénées, Occitanie, 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 |
|---|---|---|---|
| Quartz | SiO2 | 100.00% | Anatase (75.16 %), Ankerite (84.53 %), Annabergite (64.54 %), Aurichalcite (66.36 %), Bieberite (66.07 %), Pyrite (67.27 %), Brianyoungite (83.87 %), Brochantite (70.20 %), Calcite (62.43 %), Cerussite (63.56 %), Chalcophyllite (78.67 %), Chalcopyrite (67.26 %), Covellite (76.39 %), Dolomite (62.52 %), Erythrite (69.80 %), Galena (65.16 %), Glaucodot (79.17 %), Heterogenite (58.82 %), Heterosite (71.04 %), Ktenasite (78.26 %), Langite (78.01 %), Linarite (74.40 %), Malachite (61.21 %), Moorhouseite (80.00 %), Muscovite (80.32 %), Namuwite (72.60 %), Pearceite (79.22 %), Rammelsbergite (69.68 %), Ramsbeckite (77.63 %), Safflorite (68.18 %), Schulenbergite (73.58 %), Serpierite (72.17 %), Spangolite (69.77 %), Sphalerite (67.53 %), Tyrolite (74.22 %), Zircon (64.02 %) |
| Anglesite | PbSO4 | 99.98% | Brianyoungite (62.37 %), Ktenasite (70.65 %), Linarite (63.68 %), Namuwite (73.97 %), Ramsbeckite (82.89 %), Schulenbergite (69.81 %), Serpierite (65.51 %) |
| Cuprite | Cu2O | 99.97% | Chalcophyllite (64.89 %), Ktenasite (66.30 %), Langite (59.73 %), Namuwite (68.49 %), Ramsbeckite (68.42 %), Schulenbergite (64.15 %), Serpierite (55.36 %), Spangolite (60.47 %) |
| Goethite | α-Fe3+O(OH) | 99.92% | Brianyoungite (51.61 %), Ktenasite (66.30 %), Langite (50.97 %), Namuwite (63.01 %), Ramsbeckite (72.37 %), Schulenbergite (55.97 %), Serpierite (51.59 %), Spangolite (55.04 %) |
| Azurite | Cu3(CO3)2(OH)2 | 99.82% | Chalcophyllite (65.78 %), Ktenasite (53.26 %), Langite (53.49 %), Ramsbeckite (50.00 %), Serpierite (51.01 %), Spangolite (61.24 %), Tyrolite (74.56 %) |
| Smithsonite | ZnCO3 | 99.67% | Aurichalcite (54.58 %), Brianyoungite (60.22 %), Ktenasite (65.22 %), Namuwite (63.01 %), Ramsbeckite (68.42 %), Schulenbergite (55.35 %) |
| Hydrozincite | Zn5(CO3)2(OH)6 | 99.09% | Brianyoungite (62.37 %), Ktenasite (51.09 %), Namuwite (63.01 %), Ramsbeckite (69.74 %), Schulenbergite (55.97 %) |
| Aragonite | CaCO3 | 98.90% | Brianyoungite (52.69 %), Ktenasite (64.13 %), Namuwite (65.75 %), Ramsbeckite (55.26 %), Schulenbergite (57.86 %) |
| Copper | Cu | 97.93% | Chalcophyllite (51.56 %), Ktenasite (55.43 %), Namuwite (56.16 %), Ramsbeckite (53.95 %), Spangolite (52.71 %) |
| Hemimorphite | Zn4Si2O7(OH)2 · H2O | 97.91% | Aurichalcite (50.47 %), Brianyoungite (50.54 %), Ktenasite (57.61 %), Namuwite (50.68 %), Ramsbeckite (59.21 %) |
| Hematite | Fe2O3 | 88.40% | Ktenasite (56.52 %), Moorhouseite (73.33 %) |
| Silver | Ag | 83.08% | Pearceite (58.12 %), Safflorite (59.63 %) |
| Skutterudite | CoAs3 | 80.57% | Rammelsbergite (53.43 %), Safflorite (58.29 %) |
| Baryte | BaSO4 | 79.67% | Brianyoungite (50.54 %), Chalcophyllite (51.11 %), Ktenasite (56.52 %), Moorhouseite (66.67 %), Namuwite (50.68 %), Ramsbeckite (50.00 %), Tyrolite (52.96 %) |
| Sulphur | S8 | 79.18% | Namuwite (54.79 %), Ramsbeckite (53.95 %) |
| Posnjakite | Cu4(SO4)(OH)6 · H2O | 77.91% | Namuwite (52.05 %), Ramsbeckite (53.95 %) |
| Arsenopyrite | FeAsS | 71.42% | Glaucodot (71.43 %) |
| Nickeline | NiAs | 69.67% | Rammelsbergite (69.68 %) |
| Albite | Na(AlSi3O8) | 65.15% | Heterosite (65.16 %) |
| Acanthite | Ag2S | 63.96% | Pearceite (63.96 %) |
| Pyrrhotite | Fe1-xS | 60.11% | Glaucodot (60.12 %) |
| Cobaltite | CoAsS | 58.92% | Glaucodot (58.93 %) |
| Triphylite | LiFe2+PO4 | 56.83% | Heterosite (71.04 %) |
| Microcline | K(AlSi3O8) | 56.56% | Heterosite (56.56 %) |
| Pyromorphite | Pb5(PO4)3Cl | 55.26% | Ramsbeckite (55.26 %) |
| Chalcanthite | CuSO4 · 5H2O | 53.33% | Moorhouseite (53.33 %) |
| Beryl | Be3Al2(Si6O18) | 53.21% | Heterosite (66.52 %) |
| Mimetite | Pb5(AsO4)3Cl | 52.17% | Ktenasite (52.17 %) |
| Olivenite | Cu2(AsO4)(OH) | 52.00% | Chalcophyllite (52.00 %) |
| Chalcocite | Cu2S | 50.30% | Covellite (50.30 %) |
| Polybasite | [Ag6Sb2S7][Ag9CuS4] | 41.03% | Pearceite (51.30 %) |
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.