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Predictive Mineralogy

Possible unrecorded species at IGC Stop 2-4, Koashva Mt, Khibiny Massif, 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
NephelineNa3K(Al4Si4O16)99.88%Eudialyte (66.67 %), Fenaksite (87.50 %), Lamprophyllite (69.66 %), Shcherbakovite (66.67 %), Sodalite (72.78 %)
VilliaumiteNaF94.04%Fenaksite (87.50 %), Shcherbakovite (52.38 %)
QuartzSiO290.76%Microcline (81.52 %), Pectolite (50.00 %)
NatroliteNa2Al2Si3O10 · 2H2O81.46%Fenaksite (50.00 %), Lamprophyllite (62.92 %)
AlbiteNa(AlSi3O8)80.77%Eudialyte (56.20 %), Microcline (56.11 %)
AstrophylliteK2NaFe2+7Ti2Si8O26(OH)4F76.19%Fenaksite (50.00 %), Shcherbakovite (52.38 %)
Delhayelite(Na,K)10Ca5Al6Si32O80(Cl2,F2,SO4)3 · 18H2O75.00%Fenaksite (75.00 %)
LomonosoviteNa5Ti2(Si2O7)(PO4)O275.00%Fenaksite (75.00 %)
RasvumiteKFe2S375.00%Fenaksite (75.00 %)
CalciteCaCO364.31%Pectolite (64.32 %)
LobanoviteK2Na(Fe2+4Mg2Na)Ti2(Si4O12)2O2(OH)462.50%Fenaksite (62.50 %)
NatisiteNa2Ti(SiO4)O62.50%Fenaksite (62.50 %)
TitaniteCaTi(SiO4)O62.50%Fenaksite (62.50 %)
ZirsinaliteNa6(Ca,Mn2+,Fe2+)Zr(Si6O18)62.50%Fenaksite (62.50 %)
MuscoviteKAl2(AlSi3O10)(OH)261.50%Microcline (61.50 %)
MagnetiteFe2+Fe3+2O453.89%Sodalite (53.90 %)
FluorapatiteCa5(PO4)3F52.38%Shcherbakovite (52.38 %)
AenigmatiteNa4[Fe2+10Ti2]O4[Si12O36]50.00%Fenaksite (50.00 %)
AnniteKFe2+3(AlSi3O10)(OH)250.00%Fenaksite (50.00 %)
DjerfisheriteK6(Fe,Cu,Ni)25S26Cl50.00%Fenaksite (50.00 %)
IlmeniteFe2+TiO350.00%Fenaksite (50.00 %)
LorenzeniteNa2Ti2(Si2O6)O350.00%Fenaksite (50.00 %)
Barytolamprophyllite(Ba,Na)2(Na,Ti,Fe3+)4Ti2(Si2O7)2O(OH,F)40.00%Fenaksite (50.00 %)
SphaleriteZnS40.00%Fenaksite (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
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Fenaksite, Lamprophyllite
100
7 : Ultramafic igneous rocks6
31 : Thermally altered carbonate, phosphate, and iron formations2
9 : Lava/xenolith minerals (hornfels, sanidinite facies)2
26 : Hadean detrital minerals0
19 : Granitic intrusive rocks0
34 : Complex granite pegmatites0
24 : Authigenic minerals in terrestrial sediments (see also #17)0
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)0
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)0
13 : Hadean serpentinization0