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Predictive Mineralogy

Possible unrecorded species at Charsu Cu-Au deposit, Shah Wali Kot District, Kandahar, Afghanistan

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
QuartzSiO299.98%Azurite (64.09 %), Bornite (66.21 %), Chalcopyrite (67.26 %), Covellite (76.39 %), Cuprite (65.19 %), Gold (52.20 %), Malachite (61.21 %), Pyrite (67.27 %)
SphaleriteZnS66.05%Chalcopyrite (50.66 %), Covellite (64.68 %)
GalenaPbS65.97%Chalcopyrite (51.07 %), Covellite (64.18 %)
ChalcociteCu2S50.30%Covellite (50.30 %)

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
53 : Other minerals with taphonomic origins50
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]48
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]48
54 : Coal and other mine fire minerals (see also #51 and #56)13
50 : Coal and/or oil shale minerals13
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]11
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]10
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)3
15 : Black/white smoker minerals and other seafloor hydrothermal minerals3
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])3