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Predictive Mineralogy

Possible unrecorded species at Cotabambas Cu-Au deposit, Cotabambas Province, Apurímac, Peru

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
QuartzSiO299.99%Alunite (61.80 %), Anhydrite (50.95 %), Bornite (66.21 %), Chalcocite (63.99 %), Chalcopyrite (67.26 %), Epidote (69.84 %), Galena (65.16 %), Gold (52.20 %), Hematite (62.61 %), Muscovite (80.32 %), Magnetite (50.54 %), Molybdenite (66.37 %), Pyrite (67.27 %), Rutile (72.22 %), Sphalerite (67.53 %), Titanite (65.16 %)
CalciteCaCO376.84%Epidote (51.60 %), Titanite (52.17 %)
MalachiteCu2(CO3)(OH)256.19%Chalcocite (56.20 %)
KaoliniteAl2(Si2O5)(OH)451.68%Alunite (51.69 %)

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
50 : Coal and/or oil shale minerals50
54 : Coal and other mine fire minerals (see also #51 and #56)44
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)36
31 : Thermally altered carbonate, phosphate, and iron formations34
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)31
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)25
43 : Shear-induced minerals (including mylonite/slickensides)25
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])24
37 : Layered igneous intrusions and related PGE minerals22
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]21