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Predictive Mineralogy

Possible unrecorded species at Nkamouna Mine, Lomié Ultramafic complex, Lomié, Haut-Nyong, East Region, Cameroon

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
PyriteFeS299.99%Arsenopyrite (79.40 %), Asbolane (54.76 %), Carrollite (69.27 %), Chalcopyrite (75.16 %), Cubanite (82.18 %), Dolomite (58.22 %), Goethite (55.41 %), Kaolinite (52.65 %), Pentlandite (58.72 %), Pyrrhotite (80.12 %)
CalciteCaCO398.02%Asbolane (50.00 %), Dolomite (65.13 %), Maghemite (51.15 %), Montmorillonite (52.16 %), Nontronite (51.54 %)
SphaleriteZnS78.13%Arsenopyrite (55.02 %), Chalcopyrite (50.66 %), Cubanite (76.46 %), Pyrrhotite (55.40 %)
MuscoviteKAl2(AlSi3O10)(OH)276.43%Kaolinite (51.81 %), Montmorillonite (51.11 %)
GalenaPbS73.29%Arsenopyrite (53.61 %), Chalcopyrite (51.07 %), Cubanite (63.07 %)
BorniteCu5FeS470.94%Carrollite (70.95 %)
HematiteFe2O363.46%Maghemite (63.46 %)
ChalcociteCu2S54.74%Carrollite (54.75 %)
MilleriteNiS52.98%Heazlewoodite (52.99 %)
MalachiteCu2(CO3)(OH)251.19%Asbolane (51.19 %)

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
48 : Soil leaching zone minerals

Unique: Gibbsite
100
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])26
6 : Secondary asteroid phases20
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]18
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]14
37 : Layered igneous intrusions and related PGE minerals13
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)7
38 : Ophiolites5
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)5
13 : Hadean serpentinization4
17 : Marine authigenic Hadean minerals (see also #24)4