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Predictive Mineralogy

Possible unrecorded species at Kenora 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
LauriteRuS299.91%Braggite (52.05 %), Cooperite (57.50 %), Hollingworthite (63.03 %), Irarsite (67.32 %), Ruarsite (82.35 %), Rustenburgite (58.49 %), Telluropalladinite (52.00 %)
GypsumCaSO4 Β· 2H2O97.55%Copiapite (56.84 %), Halotrichite (61.51 %), Melanterite (53.56 %), Rozenite (68.37 %)
AegirineNaFe3+Si2O696.47%Ancylite-(Ce) (66.40 %), Cancrinite (57.33 %), Carbocernaite (50.00 %), Katophorite (50.82 %)
TriphyliteLiFe2+PO494.42%Alluaudite (66.04 %), Graftonite (59.84 %), Sarcopside (59.15 %)
CovelliteCuS93.59%Digenite (72.00 %), Paracostibite (50.00 %), Wittichenite (54.25 %)
VysotskitePdS84.00%Palladoarsenide (60.00 %), Telluropalladinite (60.00 %)
StrontianiteSrCO370.45%Carbocernaite (70.45 %)
MiargyriteAgSbS269.23%Zoubekite (69.23 %)
ValentiniteSb2O368.59%Senarmontite (68.60 %)
BruciteMg(OH)265.51%Iowaite (65.52 %)
ZvyagintsevitePd3Pb63.46%Atokite (63.46 %)
RhodochrositeMnCO361.61%Jacobsite (61.62 %)
CerussitePbCO360.73%Litharge (60.74 %)
Heterosite(Fe3+,Mn3+)PO455.66%Alluaudite (55.66 %)
DyscrasiteAg3Sb55.12%Allargentum (55.13 %)
AnglesitePbSO453.37%Litharge (53.37 %)
HausmanniteMn2+Mn3+2O452.52%Jacobsite (52.53 %)
IsoferroplatinumPt3Fe52.38%Menshikovite (52.38 %)
StillwateritePd8As352.38%Menshikovite (52.38 %)
KeithconnitePd20Te752.00%Telluropalladinite (52.00 %)
AnataseTiO251.40%Synchysite-(Ce) (51.41 %)
RhodoniteCaMn3Mn[Si5O15]50.00%Jacobsite (50.00 %)
CostibiteCoSbS50.00%Paracostibite (50.00 %)
SudburyitePdSb50.00%Testibiopalladite (50.00 %)
SobolevskitePdBi50.00%Atokite (50.00 %)
ErlichmaniteOsS240.00%Ruarsite (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: Allargentum, Benleonardite, Berthierite, Boulangerite, Bournonite, Calaverite, etc.
1,210
34 : Complex granite pegmatites

Unique: Eucryptite, Ferrotitanowodginite, Ferrowodginite, Fluor-liddicoatite, Spodumene, Lithiophilite, etc.
802
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Siegenite, Vaesite
100
37 : Layered igneous intrusions and related PGE minerals87
26 : Hadean detrital minerals56
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]46
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)46
35 : Ultra-alkali and agpaitic igneous rocks36
6 : Secondary asteroid phases34
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)32
36 : Carbonatites, kimberlites, and related igneous rocks24
31 : Thermally altered carbonate, phosphate, and iron formations24
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]22