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Predictive Mineralogy

Possible unrecorded species at Lower Collioux Mine, Saint-Luc, Anniviers, Sierre, 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
ChalcopyriteCuFeS299.99%Allophane (55.04 %), Annabergite (67.93 %), Arsenolite (65.02 %), Arsenopyrite (61.33 %), Atelestite (53.57 %), Beyerite (50.44 %), Bismuth (65.27 %), Bismuthinite (73.84 %), Cobaltite (85.76 %), Eclarite (72.22 %), Erythrite (69.91 %), Ferrisymplesite (66.67 %), Galenobismutite (81.11 %), Gersdorffite (83.02 %), Gladite (74.32 %), Hörnesite (68.80 %), Jarosite (50.73 %), Krupkaite (78.35 %), Löllingite (64.20 %), Mixite (63.02 %), Parasymplesite (64.54 %), Pekoite (84.44 %), Pharmacosiderite (59.35 %), Picropharmacolite (58.33 %), Preisingerite (62.30 %), Pyrite (51.72 %), Safflorite (71.66 %), Scorodite (53.74 %), Siderite (51.43 %), Skutterudite (66.89 %), Symplesite (66.02 %), Yukonite (58.82 %)
GalenaPbS99.99%Annabergite (57.37 %), Arsenolite (53.61 %), Arsenopyrite (53.61 %), Bismuth (51.78 %), Bismuthinite (57.89 %), Cobaltite (57.74 %), Eclarite (50.00 %), Erythrite (53.28 %), Ferrisymplesite (50.00 %), Galenobismutite (78.34 %), Gersdorffite (68.13 %), Gladite (63.51 %), Hörnesite (58.40 %), Krupkaite (69.07 %), Löllingite (53.52 %), Parasymplesite (55.32 %), Pekoite (71.11 %), Pharmacosiderite (51.63 %), Safflorite (59.36 %), Scorodite (50.30 %), Skutterudite (51.58 %), Symplesite (56.31 %), Wulfenite (69.21 %)
MalachiteCu2(CO3)(OH)299.30%Allophane (53.24 %), Erythrite (51.09 %), Ferrisymplesite (58.33 %), Mixite (70.31 %), Preisingerite (50.82 %), Yukonite (50.00 %)
Goethiteα-Fe3+O(OH)94.39%Ferrisymplesite (54.17 %), Mixite (51.04 %), Ranciéite (50.00 %), Yukonite (50.00 %)
DolomiteCaMg(CO3)293.03%Hörnesite (63.20 %), Kolfanite (57.14 %), Picropharmacolite (55.83 %)
PyrrhotiteFe1-xS90.27%Cobaltite (57.03 %), Galenobismutite (53.46 %), Gersdorffite (51.37 %)
MuscoviteKAl2(AlSi3O10)(OH)288.50%Ferri-taramite (50.00 %), Galenobismutite (53.00 %), Pekoite (51.11 %)
AikinitePbCuBiS381.23%Krupkaite (59.79 %), Pekoite (53.33 %)
AlbiteNa(AlSi3O8)80.00%Ferri-taramite (50.00 %), Winchite (60.00 %)
SphaleriteZnS79.99%Annabergite (52.59 %), Arsenolite (58.17 %), Arsenopyrite (55.02 %), Bismuth (53.21 %), Bismuthinite (60.27 %), Cobaltite (60.74 %), Eclarite (50.00 %), Erythrite (50.44 %), Ferrisymplesite (58.33 %), Galenobismutite (76.50 %), Gersdorffite (65.94 %), Gladite (62.16 %), Hörnesite (52.80 %), Krupkaite (64.95 %), Löllingite (59.55 %), Parasymplesite (59.57 %), Pekoite (71.11 %), Picropharmacolite (50.83 %), Safflorite (56.95 %), Symplesite (62.14 %)
MagnetiteFe2+Fe3+2O478.94%Ferri-taramite (50.00 %), Ilmenite (57.89 %)
GoldAu74.06%Galenobismutite (53.92 %), Krupkaite (61.86 %), Pekoite (57.78 %)
SilverAg72.07%Ferrisymplesite (50.00 %), Safflorite (59.63 %), Skutterudite (50.92 %)
BaryteBaSO471.80%Ferri-taramite (50.00 %), Mixite (57.81 %), Ranciéite (51.44 %)
CerussitePbCO358.77%Wulfenite (58.77 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 157.14%Kolfanite (57.14 %)
ConichalciteCaCu(AsO4)(OH)57.14%Kolfanite (57.14 %)
AzuriteCu3(CO3)2(OH)254.16%Mixite (54.17 %)
HematiteFe2O352.88%Ranciéite (52.88 %)
PharmacoliteCa(HAsO4) · 2H2O50.83%Picropharmacolite (50.83 %)
Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)250.00%Ferri-taramite (50.00 %)
TitaniteCaTi(SiO4)O50.00%Ferri-taramite (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: Gladite, Krupkaite, Pekoite, Safflorite
451
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]172
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]170
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
117
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite
100
37 : Layered igneous intrusions and related PGE minerals25
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]18
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)16
6 : Secondary asteroid phases13
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)13
34 : Complex granite pegmatites9
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)9
50 : Coal and/or oil shale minerals7