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Predictive Mineralogy

Possible unrecorded species at Praborna Mine, Saint-Marcel, Aosta Valley, 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
PyriteFeS299.99%Actinolite (62.14 %), Muscovite (50.01 %), Anatase (53.26 %), Calcite (51.16 %), Clinochlore (51.79 %), Clinozoisite (51.74 %), Epidote (56.37 %), Hematite (50.17 %), Kutnohorite (63.08 %), Neotocite (53.99 %), Pentlandite (58.72 %), Pyroxmangite (52.41 %), Rhodochrosite (56.95 %), Rutile (52.79 %), Slavíkite (66.67 %), Tremolite (57.83 %), Violarite (81.74 %)
BaryteBaSO499.71%Fluorcalcioroméite (53.33 %), Gasparite-(La) (50.00 %), Macfallite (66.67 %), Okhotskite (71.43 %), Piemontite-(Sr) (66.67 %), Tiragalloite (61.11 %)
PyrrhotiteFe1-xS94.49%Pentlandite (74.78 %), Violarite (78.17 %)
ChalcopyriteCuFeS278.25%Actinolite (52.26 %), Pentlandite (73.72 %), Violarite (82.63 %)
Clino-suenoite◻{Mn2+2}{Mg5}(Si8O22)(OH)275.00%Ferri-ghoseite (75.00 %)
TilasiteCaMg(AsO4)F75.00%Gasparite-(La) (75.00 %)
GypsumCaSO4 · 2H2O68.51%Slavíkite (68.52 %)
OrientiteCa8Mn3+10(SiO4)3(Si3O10)3(OH)10 · 4H2O 66.66%Macfallite (66.67 %)
Gasparite-(Ce)Ce(AsO4)62.50%Gasparite-(La) (62.50 %)
ChromiteFe2+Cr3+2O457.93%Uvarovite (57.94 %)
CaryopiliteMn2+3Si2O5(OH)457.14%Okhotskite (57.14 %)
Parsettensite(K,Na,Ca)7.5(Mn,Mg)49Si72O168(OH)50 · nH2O57.14%Okhotskite (57.14 %)
PrehniteCa2Al2Si3O10(OH)257.14%Okhotskite (57.14 %)
Pumpellyite-(Mn2+)Ca2Mn2+Al2(Si2O7)(SiO4)(OH)2 · H2O57.14%Okhotskite (57.14 %)
MolybdeniteMoS255.99%Powellite (55.99 %)
NephelineNa3K(Al4Si4O16)50.71%Aegirine-augite (50.72 %)
DolomiteCaMg(CO3)250.17%Kutnohorite (50.18 %)
KyaniteAl2(SiO4)O50.00%Magnesiochloritoid (50.00 %)
Manganberzeliite(NaCa2)Mn2+2(AsO4)350.00%Tiragalloite (50.00 %)
SarkiniteMn2+2(AsO4)(OH)50.00%Tiragalloite (50.00 %)
Monazite-(Ce)Ce(PO4)50.00%Gasparite-(La) (50.00 %)
Chernovite-(Y)Y(AsO4)50.00%Gasparite-(La) (62.50 %)
ScheeliteCa(WO4)48.22%Powellite (60.29 %)
MalachiteCu2(CO3)(OH)240.00%Tiragalloite (50.00 %)
PyrobelonitePbMn2+(VO4)(OH)40.00%Gasparite-(La) (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
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Ardennite-(As), Hausmannite, Kutnohorite, Manganiandrosite-(Ce)
413
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)

Unique: Okhotskite, Tiragalloite
204
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Gasparite-(La)
122
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Cerianite-(Ce)
100
31 : Thermally altered carbonate, phosphate, and iron formations42
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)29
34 : Complex granite pegmatites27
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]22
6 : Secondary asteroid phases18
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]16
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]11
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]10
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]10
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)8