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Predictive Mineralogy

Possible unrecorded species at Fossa degli Angeli Quarry, Torano 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
ChalcopyriteCuFeS299.99%Azurite (65.18 %), Bournonite (77.39 %), Colusite (74.31 %), Enargite (73.08 %), Jordanite (70.97 %), Malachite (60.66 %), Pyrite (51.72 %), Sphalerite (63.80 %), Sulvanite (54.10 %), Wurtzite (63.86 %)
GalenaPbS99.99%Bournonite (85.29 %), Colusite (72.22 %), Enargite (69.48 %), Jordanite (92.74 %), Sphalerite (74.68 %), Sulvanite (55.74 %), Wurtzite (72.95 %)
BorniteCu5FeS461.80%Colusite (61.81 %)
ArsenopyriteFeAsS55.79%Bournonite (55.79 %)
CovelliteCuS54.16%Colusite (54.17 %)
MarcasiteFeS250.00%Jordanite (50.00 %)
HematiteFe2O350.00%Nordstrandite (50.00 %)

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: Bournonite, Colusite, Enargite, Sulvanite
389
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Nordstrandite
104
48 : Soil leaching zone minerals

Unique: Gibbsite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)14
31 : Thermally altered carbonate, phosphate, and iron formations12
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]9
53 : Other minerals with taphonomic origins7
50 : Coal and/or oil shale minerals4
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)4
11 : Volcanic fumarole minerals; reduced phases (see also #45)4
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)4
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)2
36 : Carbonatites, kimberlites, and related igneous rocks2