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Predictive Mineralogy

Possible unrecorded species at No. 2 vein, Vignola Mine, Vignola-Falesina, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy

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
PyrrhotiteFe1-xS79.99%Cobaltite (57.03 %), Galenobismutite (53.46 %)
AragoniteCaCO376.84%Brianyoungite (52.69 %), Orthoserpierite (51.06 %)
BismuthiniteBi2S364.05%Galenobismutite (64.06 %)
SerpieriteCa(Cu,Zn)4(SO4)2(OH)6 · 3H2O63.82%Orthoserpierite (63.83 %)
ScoroditeFe3+AsO4 · 2H2O61.99%Pharmacosiderite (61.99 %)
TyroliteCa2Cu9(AsO4)4(CO3)(OH)8 · 11H2O57.39%Strashimirite (57.39 %)
DolomiteCaMg(CO3)252.68%Brianyoungite (52.69 %)
CopperCu51.55%Chalcophyllite (51.56 %)
BismuthBi50.69%Galenobismutite (50.69 %)
KaoliniteAl2(Si2O5)(OH)450.40%Dickite (50.40 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
GoldAu43.13%Galenobismutite (53.92 %)

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]120
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]101
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
100
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]16
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])12
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]9
37 : Layered igneous intrusions and related PGE minerals9
50 : Coal and/or oil shale minerals8
56 : Slag and smelter minerals (see also #51 and #55)8
53 : Other minerals with taphonomic origins7
55 : Anthropogenic mine minerals7