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Predictive Mineralogy

Possible unrecorded species at El Galeno Cu-Au-Mo deposit, Quisquimayoc, Celendín Province, Cajamarca, 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
SphaleriteZnS79.76%Arsenopyrite (55.02 %), Brochantite (50.32 %), Chalcopyrite (50.66 %), Covellite (64.68 %), Digenite (61.34 %), Mackinawite (57.00 %), Pyrrhotite (55.40 %)
GalenaPbS78.85%Arsenopyrite (53.61 %), Brochantite (55.97 %), 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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]50
53 : Other minerals with taphonomic origins42
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]24
50 : Coal and/or oil shale minerals18
54 : Coal and other mine fire minerals (see also #51 and #56)17
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]12
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)11
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]11
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])10
56 : Slag and smelter minerals (see also #51 and #55)10