Predictive Mineralogy
Possible unrecorded species at Kaltenberg Mine, Blüomatttälli, Turtmann Valley, Turtmann-Unterems, Leuk, Valais, Switzerland
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% | Acanthite (68.82 %), Aikinite (81.56 %), Annabergite (66.14 %), Arsenolite (71.10 %), Arsenopyrite (79.40 %), Baryte (50.79 %), Bismuth (65.41 %), Bornite (70.77 %), Brochantite (63.33 %), Chalcopyrite (75.16 %), Cobaltite (78.87 %), Eclarite (66.67 %), Epidote (56.37 %), Erythrite (64.88 %), Gersdorffite (82.91 %), Gladite (77.03 %), Glaucodot (86.31 %), Hematite (50.17 %), Hodrušite (84.38 %), Hörnesite (72.00 %), Jarosite (68.24 %), Kupčíkite (69.23 %), Langite (68.50 %), Lavendulan (59.65 %), Löllingite (66.48 %), Maucherite (61.05 %), Nickeline (66.71 %), Pearceite (80.52 %), Rammelsbergite (75.09 %), Rösslerite (69.57 %), Safflorite (68.45 %), Silver (54.72 %), Skutterudite (62.40 %), Sphalerite (75.10 %), Sulphur (55.07 %), Uraninite (51.44 %) |
Quartz | SiO2 | 100.00% | Acanthite (72.42 %), Aikinite (84.42 %), Albite (78.81 %), Annabergite (64.54 %), Aragonite (53.70 %), Arsenolite (75.29 %), Arsenopyrite (80.07 %), Baryte (60.21 %), Bismuth (78.36 %), Bornite (66.21 %), Brochantite (70.20 %), Cassiterite (58.88 %), Chalcopyrite (67.26 %), Cobaltite (70.11 %), Eclarite (66.67 %), Epidote (69.84 %), Erythrite (69.80 %), Fluorapatite (70.90 %), Gersdorffite (75.25 %), Gladite (79.73 %), Glaucodot (79.17 %), Hematite (62.61 %), Hodrušite (87.50 %), Hörnesite (77.60 %), Ilmenite (52.06 %), Jarosite (68.17 %), Kupčíkite (84.62 %), Langite (78.01 %), Lavendulan (70.18 %), Löllingite (76.36 %), Magnetite (50.54 %), Nickeline (58.64 %), Pearceite (79.22 %), Rammelsbergite (69.68 %), Rösslerite (91.30 %), Safflorite (68.18 %), Silver (59.03 %), Skutterudite (59.90 %), Sphalerite (67.53 %), Sulphur (53.86 %), Uraninite (52.94 %) |
Galena | PbS | 99.99% | Acanthite (69.24 %), Aikinite (80.78 %), Annabergite (57.37 %), Arsenolite (53.61 %), Arsenopyrite (53.61 %), Bismuth (51.78 %), Brochantite (55.97 %), Chalcopyrite (51.07 %), Cobaltite (57.74 %), Eclarite (50.00 %), Erythrite (53.28 %), Gersdorffite (68.13 %), Gladite (63.51 %), Glaucodot (70.83 %), Hodrušite (71.88 %), Hörnesite (58.40 %), Kupčíkite (61.54 %), Langite (63.00 %), Lavendulan (54.39 %), Löllingite (53.52 %), Nickeline (55.15 %), Pearceite (84.09 %), Rammelsbergite (64.62 %), Rösslerite (56.52 %), Safflorite (59.36 %), Silver (52.62 %), Skutterudite (51.58 %), Sphalerite (74.68 %) |
Calcite | CaCO3 | 99.99% | Acanthite (51.71 %), Aikinite (51.95 %), Annabergite (60.16 %), Aragonite (71.64 %), Arsenolite (61.98 %), Baryte (51.88 %), Brochantite (53.68 %), Cobaltite (51.81 %), Epidote (51.60 %), Erythrite (59.85 %), Gersdorffite (53.89 %), Glaucodot (58.93 %), Hodrušite (62.50 %), Hörnesite (78.40 %), Jarosite (50.12 %), Kupčíkite (53.85 %), Langite (60.92 %), Lavendulan (66.67 %), Löllingite (51.02 %), Nickeline (56.82 %), Pearceite (61.04 %), Rammelsbergite (70.76 %), Rösslerite (65.22 %), Safflorite (66.31 %), Skutterudite (59.07 %) |
Malachite | Cu2(CO3)(OH)2 | 99.90% | Brochantite (75.59 %), Erythrite (51.09 %), Kupčíkite (53.85 %), Langite (85.29 %), Lavendulan (70.18 %), Rösslerite (60.87 %) |
Bismuthinite | Bi2S3 | 99.59% | Eclarite (61.11 %), Gladite (68.92 %), Hodrušite (78.13 %), Kupčíkite (84.62 %) |
Pyrrhotite | Fe1-xS | 96.27% | Cobaltite (57.03 %), Gersdorffite (51.37 %), Glaucodot (60.12 %), Maucherite (55.26 %) |
Dolomite | CaMg(CO3)2 | 90.39% | Hörnesite (63.20 %), Rösslerite (73.91 %) |
Emplectite | CuBiS2 | 83.17% | Hodrušite (56.25 %), Kupčíkite (61.54 %) |
Azurite | Cu3(CO3)2(OH)2 | 77.69% | Langite (53.49 %), Lavendulan (52.05 %) |
Gold | Au | 74.57% | Aikinite (52.99 %), Hodrušite (68.75 %), Kupčíkite (53.85 %) |
Pharmacolite | Ca(HAsO4) · 2H2O | 69.56% | Rösslerite (69.57 %) |
Nickelskutterudite | (Ni,Co,Fe)As3 | 65.21% | Rösslerite (65.22 %) |
Picropharmacolite | Ca4Mg(AsO4)2(HAsO4)2 · 11H2O | 65.21% | Rösslerite (65.22 %) |
Proustite | Ag3AsS3 | 65.21% | Rösslerite (65.22 %) |
Cuprite | Cu2O | 59.73% | Langite (59.73 %) |
Olivenite | Cu2(AsO4)(OH) | 58.47% | Lavendulan (58.48 %) |
Pentlandite | (NixFey)Σ9S8 | 58.42% | Maucherite (58.42 %) |
Arsenic | As | 56.52% | Rösslerite (56.52 %) |
Realgar | As4S4 | 56.52% | Rösslerite (56.52 %) |
Cerussite | PbCO3 | 53.93% | Langite (53.94 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 52.79% | Albite (52.80 %) |
Pyrargyrite | Ag3SbS3 | 52.17% | Rösslerite (52.17 %) |
Polybasite | [Ag6Sb2S7][Ag9CuS4] | 51.29% | Pearceite (51.30 %) |
Goethite | α-Fe3+O(OH) | 50.96% | Langite (50.97 %) |
Chalcocite | Cu2S | 50.00% | Hodrušite (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.