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Predictive Mineralogy

Possible unrecorded species at Severny area, Malyi Murun Massif (Malomurunskiy; Maly Murun alkaline pluton; Malyy Murun massif), Irkutsk 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
ChalcopyriteCuFeS299.99%Chalcocite (74.77 %), Copper (53.15 %), Covellite (85.83 %), Digenite (87.06 %), Galena (56.79 %), Idaite (91.20 %)
PyriteFeS299.98%Baryte (50.79 %), Calcite (51.16 %), Chalcocite (65.95 %), Covellite (80.77 %), Digenite (79.44 %), Galena (66.84 %), Idaite (77.36 %), Wollastonite (51.22 %)
MalachiteCu2(CO3)(OH)296.33%Chalcocite (56.20 %), Covellite (54.66 %), Digenite (54.15 %), Idaite (59.75 %)
BorniteCu5FeS495.02%Digenite (68.36 %), Idaite (84.28 %)
SphaleriteZnS78.71%Covellite (64.68 %), Digenite (61.34 %), Galena (65.95 %), Idaite (65.41 %)
MuscoviteKAl2(AlSi3O10)(OH)261.50%Microcline (61.50 %)
AlbiteNa(AlSi3O8)56.11%Microcline (56.11 %)
TinaksiteK2Na(Ca,Mn2+)2TiO[Si7O18(OH)]55.38%Charoite (69.23 %)
DiopsideCaMgSi2O650.54%Wollastonite (50.54 %)

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
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Charoite, Fluorcarletonite
100
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])6
6 : Secondary asteroid phases6
19 : Granitic intrusive rocks1
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)1
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)1
34 : Complex granite pegmatites1
26 : Hadean detrital minerals0
24 : Authigenic minerals in terrestrial sediments (see also #17)0
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)0
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]0