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Predictive Mineralogy

Possible unrecorded species at Mt Cleveland Mine, Luina, Heazlewood district, Waratah-Wynyard municipality, Tasmania, Australia

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
BerylBe3Al2(Si6O18)94.55%Bavenite (51.21 %), Bertrandite (63.34 %), Morinite (69.57 %)
FluorapatiteCa5(PO4)3F90.33%Morinite (78.26 %), Tetrawickmanite (55.56 %)
MalachiteCu2(CO3)(OH)280.13%Chalcocite (56.20 %), Covellite (54.66 %)
MicroclineK(AlSi3O8)77.77%Tetrawickmanite (77.78 %)
NatroliteNa2Al2Si3O10 · 2H2O77.77%Tetrawickmanite (77.78 %)
TitaniteCaTi(SiO4)O75.68%Bavenite (50.52 %), Hastingsite (50.85 %)
AnalcimeNa(AlSi2O6) · H2O66.66%Tetrawickmanite (66.67 %)
Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O66.66%Tetrawickmanite (66.67 %)
HambergiteBe2(BO3)(OH)66.66%Tetrawickmanite (66.67 %)
HelvineBe3Mn2+4(SiO4)3S66.66%Tetrawickmanite (66.67 %)
Neotocite(Mn,Fe,Mg)SiO3 · H2O66.66%Tetrawickmanite (66.67 %)
AegirineNaFe3+Si2O655.55%Tetrawickmanite (55.56 %)
EpididymiteNa2Be2Si6O15 · H2O55.55%Tetrawickmanite (55.56 %)
Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2O55.55%Tetrawickmanite (55.56 %)
Meliphanite(Ca,Na)2(Be,Al)[Si2O6(OH,F)]55.55%Tetrawickmanite (55.56 %)
Thomsonite-CaNaCa2[Al5Si5O20] · 6H2O55.55%Tetrawickmanite (55.56 %)
ZirconZr(SiO4)53.33%Tetrawickmanite (66.67 %)
DiopsideCaMgSi2O650.54%Wollastonite (50.54 %)
KaoliniteAl2(Si2O5)(OH)450.40%Dickite (50.40 %)

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
34 : Complex granite pegmatites

Unique: Luinaite-(OH)
142
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
100
31 : Thermally altered carbonate, phosphate, and iron formations26
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)24
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)20
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]20
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)13
26 : Hadean detrital minerals12
35 : Ultra-alkali and agpaitic igneous rocks10
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])8
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits8
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]6