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Predictive Mineralogy

Possible unrecorded species at Koidu-Yengema, Kono District, Eastern Province, Sierra Leone

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
TroiliteFeS71.01%Iron (71.02 %)
ChalcopyriteCuFeS270.81%Pyrite (51.72 %), Pyrrhotite (76.22 %)
Taenite(Fe,Ni)59.57%Iron (59.58 %)
MuscoviteKAl2(AlSi3O10)(OH)256.04%Almandine (56.05 %)
SphaleriteZnS44.31%Pyrrhotite (55.40 %)
ChromiteFe2+Cr3+2O440.94%Iron (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
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Titanomaghemite
100
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)8
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)8
6 : Secondary asteroid phases6
36 : Carbonatites, kimberlites, and related igneous rocks5
26 : Hadean detrital minerals5
38 : Ophiolites3
7 : Ultramafic igneous rocks3
8 : Mafic igneous rocks2
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])2
42 : Sea-floor Mn nodules2