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Predictive Mineralogy

Possible unrecorded species at Henderson mine, Opemisca deposits, Chibougamau, Jamésie, Nord-du-Québec, Québec, 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
GalenaPbS79.94%Ankerite (54.09 %), Arsenopyrite (53.61 %), Chalcopyrite (51.07 %), Cobaltite (57.74 %), Siegenite (68.94 %), Sphalerite (74.68 %), Willyamite (80.00 %)
UllmanniteNiSbS70.00%Willyamite (70.00 %)
MalachiteCu2(CO3)(OH)256.19%Chalcocite (56.20 %)
MilleriteNiS51.19%Siegenite (51.19 %)
GoldAu50.66%Willyamite (63.33 %)
MarcasiteFeS250.00%Willyamite (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: Willyamite
112
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Siegenite
100
37 : Layered igneous intrusions and related PGE minerals13
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)7
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)6
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)4
31 : Thermally altered carbonate, phosphate, and iron formations3
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)2
43 : Shear-induced minerals (including mylonite/slickensides)1
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)1
36 : Carbonatites, kimberlites, and related igneous rocks1
41 : Mantle metasomatism1