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Predictive Mineralogy

Possible unrecorded species at Avino Mine, Pánuco de Coronado, Pánuco de Coronado Municipality, Durango, Mexico

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%Acanthite (72.42 %), Azurite (64.09 %), Bornite (66.21 %), Chalcopyrite (67.26 %), Galena (65.16 %), Goethite (66.86 %), Gold (52.20 %), Malachite (61.21 %), Silver (59.03 %)
PyriteFeS299.97%Acanthite (68.82 %), Azurite (58.39 %), Bornite (70.77 %), Chalcopyrite (75.16 %), Galena (66.84 %), Goethite (55.41 %), Malachite (52.79 %), Silver (54.72 %)
SphaleriteZnS75.00%Acanthite (62.85 %), Chalcopyrite (50.66 %), Galena (65.95 %)
CalciteCaCO351.71%Acanthite (51.71 %)

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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])50
49 : Oxic cellular biomineralization (see also #44)47
53 : Other minerals with taphonomic origins28
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]28
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]27
36 : Carbonatites, kimberlites, and related igneous rocks4
38 : Ophiolites3
7 : Ultramafic igneous rocks3
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]3
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)1