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Predictive Mineralogy

Possible unrecorded species at Chibaisong Cu-Ni-PGE deposit, Tonghua Co., Tonghua, Jilin, China

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
CalciteCaCO399.21%Clinochlore (54.46 %), Marcasite (60.67 %), Millerite (53.62 %), Phlogopite (55.90 %), Tremolite (55.93 %), Valleriite (51.25 %)
KotulskitePd(Te,Bi)2-x (x ≈ 0.4)91.00%Merenskyite (53.06 %), Michenerite (55.19 %), Moncheite (57.22 %)
AltaitePbTe56.79%Melonite (56.79 %)
CubaniteCuFe2S356.27%Valleriite (56.27 %)
MalachiteCu2(CO3)(OH)256.19%Chalcocite (56.20 %)
GypsumCaSO4 · 2H2O50.28%Sulphur (50.28 %)
ChromiteFe2+Cr3+2O445.60%Awaruite (57.00 %)

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: Hessite
100
37 : Layered igneous intrusions and related PGE minerals34
13 : Hadean serpentinization10
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)10
7 : Ultramafic igneous rocks10
31 : Thermally altered carbonate, phosphate, and iron formations10
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]9
6 : Secondary asteroid phases5
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)4
38 : Ophiolites2
36 : Carbonatites, kimberlites, and related igneous rocks2