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Predictive Mineralogy

Possible unrecorded species at Kikonkula prospect, Lake Mweru, Pweto Territory, Haut-Katanga, DR Congo

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
PyriteFeS299.94%Baryte (50.79 %), Bornite (70.77 %), Chalcopyrite (75.16 %), Covellite (80.77 %), Digenite (79.44 %), Dolomite (58.22 %)
CalciteCaCO391.99%Baryte (51.88 %), Digenite (52.28 %), Dolomite (65.13 %)
ChalcociteCu2S82.80%Covellite (50.30 %), Digenite (65.40 %)
MalachiteCu2(CO3)(OH)279.20%Covellite (54.66 %), Digenite (54.15 %)
SphaleriteZnS74.61%Chalcopyrite (50.66 %), Covellite (64.68 %), Digenite (61.34 %)
GalenaPbS74.38%Chalcopyrite (51.07 %), Covellite (64.18 %), Digenite (59.98 %)

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
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)50
15 : Black/white smoker minerals and other seafloor hydrothermal minerals50
6 : Secondary asteroid phases41
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])39
50 : Coal and/or oil shale minerals39
54 : Coal and other mine fire minerals (see also #51 and #56)39
53 : Other minerals with taphonomic origins38
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]32
8 : Mafic igneous rocks31
34 : Complex granite pegmatites22