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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 speciesFormulaMatch %Due to recorded presence of
PyriteFeS2100.00%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 %)
QuartzSiO2100.00%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 %)
GalenaPbS99.99%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 %)
CalciteCaCO399.99%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 %)
MalachiteCu2(CO3)(OH)299.90%Brochantite (75.59 %), Erythrite (51.09 %), Kupčíkite (53.85 %), Langite (85.29 %), Lavendulan (70.18 %), Rösslerite (60.87 %)
BismuthiniteBi2S399.59%Eclarite (61.11 %), Gladite (68.92 %), Hodrušite (78.13 %), Kupčíkite (84.62 %)
PyrrhotiteFe1-xS96.27%Cobaltite (57.03 %), Gersdorffite (51.37 %), Glaucodot (60.12 %), Maucherite (55.26 %)
DolomiteCaMg(CO3)290.39%Hörnesite (63.20 %), Rösslerite (73.91 %)
EmplectiteCuBiS283.17%Hodrušite (56.25 %), Kupčíkite (61.54 %)
AzuriteCu3(CO3)2(OH)277.69%Langite (53.49 %), Lavendulan (52.05 %)
GoldAu74.57%Aikinite (52.99 %), Hodrušite (68.75 %), Kupčíkite (53.85 %)
PharmacoliteCa(HAsO4) · 2H2O69.56%Rösslerite (69.57 %)
Nickelskutterudite(Ni,Co,Fe)As365.21%Rösslerite (65.22 %)
PicropharmacoliteCa4Mg(AsO4)2(HAsO4)2 · 11H2O65.21%Rösslerite (65.22 %)
ProustiteAg3AsS365.21%Rösslerite (65.22 %)
CupriteCu2O59.73%Langite (59.73 %)
OliveniteCu2(AsO4)(OH)58.47%Lavendulan (58.48 %)
Pentlandite(NixFey)Σ9S858.42%Maucherite (58.42 %)
ArsenicAs56.52%Rösslerite (56.52 %)
RealgarAs4S456.52%Rösslerite (56.52 %)
CerussitePbCO353.93%Langite (53.94 %)
MuscoviteKAl2(AlSi3O10)(OH)252.79%Albite (52.80 %)
PyrargyriteAg3SbS352.17%Rösslerite (52.17 %)
Polybasite[Ag6Sb2S7][Ag9CuS4]51.29%Pearceite (51.30 %)
Goethiteα-Fe3+O(OH)50.96%Langite (50.97 %)
ChalcociteCu2S50.00%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.

Paragenetic ModeScore
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Aikinite, Gladite, Glaucodot, Hodrušite, Maucherite, Pearceite, etc.
864
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]46
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]43
37 : Layered igneous intrusions and related PGE minerals38
49 : Oxic cellular biomineralization (see also #44)14
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)13
55 : Anthropogenic mine minerals7
34 : Complex granite pegmatites6
38 : Ophiolites5
36 : Carbonatites, kimberlites, and related igneous rocks5
50 : Coal and/or oil shale minerals5