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Predictive Mineralogy

Possible unrecorded species at Is River, Nizhnyaya Tura, Sverdlovsk Oblast, Russia

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
ChromiteFe2+Cr3+2O493.66%Cuproiridsite (62.50 %), Malanite (57.78 %), Tetraferroplatinum (60.00 %)
PseudobrookiteFe2TiO580.00%Naquite (100.00 %)
LauriteRuS279.59%Cuproiridsite (90.00 %), Isoferroplatinum (55.23 %), Malanite (73.33 %), Tetraferroplatinum (57.65 %)
QuartzSiO277.08%Cinnabar (52.07 %), Gold (52.20 %)
SperrylitePtAs275.21%Isoferroplatinum (52.33 %), Malanite (64.44 %), Tetraferroplatinum (64.71 %)
LinzhiiteFeSi266.66%Naquite (66.67 %)
ErlichmaniteOsS262.50%Cuproiridsite (62.50 %)
CooperitePtS62.22%Malanite (62.22 %)
MagnetiteFe2+Fe3+2O456.47%Tetraferroplatinum (56.47 %)
Iridium(Ir,Os,Ru)52.07%Osmium (52.07 %)
Cuprorhodsite(Cu1+0.5Fe3+0.5)Rh3+2S448.00%Cuproiridsite (60.00 %)
Irarsite(Ir,Ru,Rh,Pt)AsS44.00%Cuproiridsite (55.00 %)
Pentlandite(NixFey)Σ9S843.29%Tetraferroplatinum (54.12 %)
Hollingworthite(Rh,Pt,Pd)AsS40.88%Malanite (51.11 %)

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
7 : Ultramafic igneous rocks

Unique: Tongbaite
100
26 : Hadean detrital minerals37
6 : Secondary asteroid phases10
37 : Layered igneous intrusions and related PGE minerals8
38 : Ophiolites6
36 : Carbonatites, kimberlites, and related igneous rocks5
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)3
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])3
5 : Primary asteroid phases3
56 : Slag and smelter minerals (see also #51 and #55)1
11 : Volcanic fumarole minerals; reduced phases (see also #45)1