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Predictive Mineralogy

Possible unrecorded species at Kolmozero-Voronye belt, Kola Peninsula, Murmansk 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
CalciteCaCO399.99%Acanthite (51.71 %), Bavenite (51.90 %), Boulangerite (52.73 %), Calaverite (51.83 %), Cervelleite (50.00 %), Cobaltite (51.81 %), Diaphorite (54.14 %), Diopside (54.07 %), Dyscrasite (63.35 %), Epidote (51.60 %), Fizélyite (54.84 %), Greenockite (70.86 %), Hydroxycalciopyrochlore (72.22 %), Löllingite (51.02 %), Marcasite (60.67 %), Mckinstryite (69.44 %), Petzite (51.11 %), Ramdohrite (50.00 %), Semseyite (55.66 %), Stephanite (54.56 %), Symplesite (52.43 %), Ullmannite (56.15 %), Uytenbogaardtite (53.03 %)
StibniteSb2S396.48%Aurostibite (58.06 %), Fizélyite (51.61 %), Ramdohrite (62.50 %), Semseyite (53.77 %)
BournonitePbCuSbS382.53%Fizélyite (54.84 %), Semseyite (61.32 %)
MiargyriteAgSbS280.12%Fizélyite (53.23 %), Ramdohrite (57.50 %)
FluoriteCaF276.64%Bavenite (53.29 %), Hydroxycalciopyrochlore (50.00 %)
CerussitePbCO368.60%Pyromorphite (68.61 %)
AltaitePbTe65.59%Stützite (65.60 %)
TopazAl2(SiO4)(F,OH)263.15%Fluornatromicrolite (63.16 %)
ScoroditeFe3+AsO4 · 2H2O63.10%Symplesite (63.11 %)
BismuthiniteBi2S360.00%Bismite (60.00 %)
StromeyeriteAgCuS59.72%Mckinstryite (59.72 %)
BerauniteFe3+6(PO4)4O(OH)4 · 6H2O57.14%Lithiophosphate (57.14 %)
FairfielditeCa2Mn2+(PO4)2 · 2H2O57.14%Lithiophosphate (57.14 %)
WhitlockiteCa9Mg(PO4)6(PO3OH)57.14%Lithiophosphate (57.14 %)
MalachiteCu2(CO3)(OH)254.65%Covellite (54.66 %)
SylvaniteAgAuTe451.20%Stützite (51.20 %)
TitaniteCaTi(SiO4)O50.51%Bavenite (50.52 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
HematiteFe2O350.00%Hydroxycalciopyrochlore (50.00 %)
ThoriteTh(SiO4)48.88%Hydroxycalciopyrochlore (61.11 %)
BaryteBaSO440.00%Ramdohrite (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: Boulangerite, Calaverite, Cervelleite, Diaphorite, Dyscrasite, Fizélyite, etc.
1,936
34 : Complex granite pegmatites

Unique: Eucryptite, Fluornatromicrolite, Ixiolite-(Mn2+)-Ixiolite-(Fe2+) Series, Lithiophilite, Microlite Group, Simpsonite, etc.
1,091
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Uchucchacuaite
104
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
103
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite
100
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)38
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]30
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)29
35 : Ultra-alkali and agpaitic igneous rocks27
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]25
26 : Hadean detrital minerals19
49 : Oxic cellular biomineralization (see also #44)14
37 : Layered igneous intrusions and related PGE minerals14
6 : Secondary asteroid phases13
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]8