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Predictive Mineralogy

Possible unrecorded species at Sikhote-Alin Mountains, 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
ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)92.68%Rossmanite (85.37 %), Viitaniemiite (50.00 %)
MerenskyitePdTe291.01%Kotulskite (62.28 %), Sopcheite (76.19 %)
MoncheitePt(Te,Bi)289.96%Kotulskite (61.68 %), Sopcheite (73.81 %)
PyrolusiteMn4+O289.70%Akhtenskite (71.43 %), Manganite (63.98 %)
EnargiteCu3AsS488.33%Goldfieldite (57.47 %), Luzonite (72.57 %)
MimetitePb5(AsO4)3Cl81.42%Adamite (58.67 %), Köttigite (55.07 %)
AikinitePbCuBiS378.57%Berryite (57.14 %), Mummeite (50.00 %)
PetziteAg3AuTe277.42%Coloradoite (54.85 %), Kurilite (50.00 %)
Bixbyite-(Mn)Mn3+2O377.27%Ephesite (77.27 %)
MicheneritePdBiTe76.61%Kotulskite (50.90 %), Sopcheite (52.38 %)
LauriteRuS267.31%Irarsite (67.32 %)
UraniniteUO265.15%Kasolite (65.16 %)
UmangiteCu3Se262.33%Klockmannite (62.34 %)
NephelineNa3K(Al4Si4O16)60.65%Rhönite (60.66 %)
UranophaneCa(UO2)2(SiO3OH)2 · 5H2O60.18%Kasolite (60.18 %)
MaldoniteAu2Bi58.33%Jonassonite (58.33 %)
AragoniteCaCO357.97%Köttigite (57.97 %)
GypsumCaSO4 · 2H2O57.97%Köttigite (57.97 %)
CryptomelaneK(Mn4+7Mn3+)O1657.14%Akhtenskite (57.14 %)
Nsutite(Mn4+,Mn2+)(O,OH)257.14%Akhtenskite (57.14 %)
BrauniteMn2+Mn3+6(SiO4)O855.55%Kanoite (55.56 %)
AnglesitePbSO455.07%Köttigite (55.07 %)
Columbite-(Mn)Mn2+Nb2O653.65%Rossmanite (53.66 %)
BerzelianiteCu2-xSe (x ≈ 0.12)53.24%Klockmannite (53.25 %)
TriphyliteLiFe2+PO453.12%Triploidite (53.13 %)
MixiteBiCu6(AsO4)3(OH)6 · 3H2O52.45%Preisingerite (52.46 %)
TelluriumTe51.51%Tellurite (51.52 %)
HemimorphiteZn4Si2O7(OH)2 · H2O50.46%Aurichalcite (50.47 %)
CostibiteCoSbS50.00%Paracostibite (50.00 %)
VysotskitePdS50.00%Sopcheite (50.00 %)
VivianiteFe2+Fe2+2(PO4)2 · 8H2O50.00%Triploidite (50.00 %)
Tantalite-(Mn)Mn2+Ta2O650.00%Viitaniemiite (50.00 %)
Hollingworthite(Rh,Pt,Pd)AsS40.00%Sopcheite (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: Aguilarite, Allargentum, Argyrodite, Arsenic, Babkinite, Benjaminite, etc.
4,789
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Dzhalindite, Halloysite, Natanite
386
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Johannsenite, Kutnohorite, Pyrosmalite-(Fe)
311
34 : Complex granite pegmatites

Unique: Ixiolite-(Mn2+)-Ixiolite-(Fe2+) Series, Microlite Group
284
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Gustavite, Indite, Luzonite
277
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Amesite, Minnesotaite
246
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite, Iodargyrite
169
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite
133
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
121
5 : Primary asteroid phases

Unique: Carlsbergite
109
7 : Ultramafic igneous rocks

Unique: Mariinskite
100
31 : Thermally altered carbonate, phosphate, and iron formations88
26 : Hadean detrital minerals75
37 : Layered igneous intrusions and related PGE minerals72
6 : Secondary asteroid phases68
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)57
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]48
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)44
38 : Ophiolites40
35 : Ultra-alkali and agpaitic igneous rocks26
36 : Carbonatites, kimberlites, and related igneous rocks24