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Predictive Mineralogy

Possible unrecorded species at 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)699.93%Chalcophyllite (68.89 %), Claraite (63.27 %), Connellite (68.10 %), Cornubite (61.54 %), Cualstibite (66.67 %), Lavendulan (50.29 %), Parnauite (73.60 %)
AnglesitePbSO493.32%Cualstibite (66.67 %), Fraipontite (56.45 %), Rosasite (54.03 %)
CopperCu90.26%Chalcophyllite (51.56 %), Connellite (59.48 %), Parnauite (50.40 %)
CassiteriteSnO288.82%KĂ«sterite (55.32 %), Mushistonite (75.00 %)
BismuthiniteBi2S381.90%Cannizzarite (56.52 %), Cosalite (58.38 %)
LangiteCu4(SO4)(OH)6 · 2H2O79.37%Cualstibite (55.56 %), Parnauite (53.60 %)
PyrolusiteMn4+O263.98%Manganite (63.98 %)
StanniteCu2FeSnS462.76%KĂ«sterite (62.77 %)
MicroclineK(AlSi3O8)62.50%Mushistonite (62.50 %)
GoldAu61.47%Aikinite (52.99 %), Famatinite (50.75 %)
Chernovite-(Y)Y(AsO4)60.00%Gasparite-(Ce) (75.00 %)
CornwalliteCu5(AsO4)2(OH)457.69%Cornubite (57.69 %)
MilleriteNiS55.90%Vaesite (55.91 %)
KaoliniteAl2(Si2O5)(OH)455.55%Cualstibite (55.56 %)
LinaritePbCu(SO4)(OH)255.55%Cualstibite (55.56 %)
PosnjakiteCu4(SO4)(OH)6 · H2O55.55%Cualstibite (55.56 %)
BerylBe3Al2(Si6O18)40.00%Mushistonite (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: Aikinite, Boulangerite, Bournonite, Colusite, Cosalite, Enargite, etc.
1,121
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Fraipontite, Halloysite, Nordstrandite
446
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Famatinite, KĂ«sterite, Luzonite, Vaesite
383
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
131
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Zaccagnaite
114
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
104
48 : Soil leaching zone minerals

Unique: Gibbsite
100
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]96
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]36
34 : Complex granite pegmatites31
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)29
26 : Hadean detrital minerals21
31 : Thermally altered carbonate, phosphate, and iron formations16
50 : Coal and/or oil shale minerals15
6 : Secondary asteroid phases14
46 : Near-surface hydrothermal alteration of minerals (see also #22)11
53 : Other minerals with taphonomic origins11