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Predictive Mineralogy

Possible unrecorded species at Gioia quarries, Colonnata, Colonnata quarrying basin, Carrara, Massa-Carrara Province, Tuscany, 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
BrochantiteCu4(SO4)(OH)699.52%Chalcophyllite (68.89 %), Claraite (63.27 %), Connellite (68.10 %), Lavendulan (50.29 %), Parnauite (73.60 %)
CupriteCu2O98.60%Chalcophyllite (64.89 %), Claraite (59.18 %), Connellite (72.41 %), Parnauite (64.80 %)
ArsenopyriteFeAsS97.44%Boulangerite (64.45 %), Bournonite (55.79 %), Semseyite (59.91 %), Zinkenite (59.48 %)
CopperCu90.26%Chalcophyllite (51.56 %), Connellite (59.48 %), Parnauite (50.40 %)
MimetitePb5(AsO4)3Cl90.12%Adamite (58.67 %), Claraite (51.02 %), Parnauite (51.20 %)
SmithsoniteZnCO379.82%Aurichalcite (54.58 %), Hemimorphite (55.59 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 179.44%Conichalcite (50.59 %), Parnauite (58.40 %)
PyrrhotiteFe1-xS58.69%Smythite (58.70 %)
LangiteCu4(SO4)(OH)6 · 2H2O53.60%Parnauite (53.60 %)

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])

Unique: Boulangerite, Bournonite, Colusite, Enargite, Semseyite, Sulvanite, etc.
619
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Nordstrandite
153
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Luzonite
100
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]49
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]23
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)13
6 : Secondary asteroid phases12
46 : Near-surface hydrothermal alteration of minerals (see also #22)11
53 : Other minerals with taphonomic origins9
50 : Coal and/or oil shale minerals8
54 : Coal and other mine fire minerals (see also #51 and #56)5
11 : Volcanic fumarole minerals; reduced phases (see also #45)5
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]5