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Predictive Mineralogy

Possible unrecorded species at Kerr Lake Mine (Jacobs Mine), Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada

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
QuartzSiO299.99%Acanthite (72.42 %), Allargentum (69.23 %), Antimony (74.33 %), Arsenopyrite (80.07 %), Bismuth (78.36 %), Calcite (62.43 %), Dyscrasite (71.04 %), Löllingite (76.36 %), Safflorite (68.18 %), Silver (59.03 %), Skutterudite (59.90 %), Stephanite (72.65 %)
PyriteFeS299.99%Acanthite (68.82 %), Allargentum (74.36 %), Antimony (68.52 %), Arsenopyrite (79.40 %), Bismuth (65.41 %), Calcite (51.16 %), Dyscrasite (72.40 %), Löllingite (66.48 %), Safflorite (68.45 %), Silver (54.72 %), Skutterudite (62.40 %), Stephanite (69.85 %)
PyrrhotiteFe1-xS83.81%Allargentum (61.54 %), Dyscrasite (57.92 %)
PyrargyriteAg3SbS382.74%Allargentum (58.97 %), Stephanite (57.94 %)
CinnabarHgS80.23%Mercury (80.24 %)
ChalcopyriteCuFeS279.99%Acanthite (62.06 %), Allargentum (76.92 %), Antimony (60.77 %), Arsenopyrite (61.33 %), Bismuth (65.27 %), Dyscrasite (74.66 %), Löllingite (64.20 %), Safflorite (71.66 %), Silver (50.22 %), Skutterudite (66.89 %), Stephanite (63.38 %)
GalenaPbS79.99%Acanthite (69.24 %), Allargentum (78.21 %), Antimony (54.72 %), Arsenopyrite (53.61 %), Bismuth (51.78 %), Dyscrasite (76.92 %), Löllingite (53.52 %), Safflorite (59.36 %), Silver (52.62 %), Skutterudite (51.58 %), Stephanite (71.18 %)
SphaleriteZnS79.99%Acanthite (62.85 %), Allargentum (82.05 %), Antimony (62.23 %), Arsenopyrite (55.02 %), Bismuth (53.21 %), Dyscrasite (77.38 %), Löllingite (59.55 %), Safflorite (56.95 %), Stephanite (65.44 %)
StibniteSb2S356.41%Antimony (56.42 %)

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: Allargentum, Dyscrasite, Safflorite, Stephanite
100
49 : Oxic cellular biomineralization (see also #44)3
54 : Coal and other mine fire minerals (see also #51 and #56)1
50 : Coal and/or oil shale minerals1
34 : Complex granite pegmatites1
36 : Carbonatites, kimberlites, and related igneous rocks1
38 : Ophiolites1
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)1
6 : Secondary asteroid phases1
14 : Hot springs, geysers, and other subaerial geothermal minerals1
7 : Ultramafic igneous rocks0