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Predictive Mineralogy

Possible unrecorded species at Kara No. 1 Pit, Kara Mines, Hampshire mining district, Burnie City, 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
GalenaPbS99.99%Aikinite (80.78 %), Baileychlore (78.95 %), Bismuthinite (57.89 %), Cerussite (83.05 %), Chalcopyrite (51.07 %), Greenockite (85.56 %), Helvine (50.18 %), Hemimorphite (75.39 %), Hydrozincite (82.83 %), Ilvaite (57.39 %), Mimetite (75.78 %), Pyromorphite (77.81 %), Rosasite (78.02 %), Sphalerite (74.68 %), Stolzite (71.19 %), Wulfenite (69.21 %)
AlbiteNa(AlSi3O8)97.88%Bavenite (70.59 %), Danalite (54.67 %), Helvine (56.73 %), Milarite (63.37 %)
SmithsoniteZnCO392.87%Hemimorphite (55.59 %), Hydrozincite (62.08 %), Rosasite (57.69 %)
Hydrokenoelsmoreite2W2O6(H2O)90.66%Anthoinite (53.33 %), Mpororoite (80.00 %)
MuscoviteKAl2(AlSi3O10)(OH)278.34%Bavenite (55.71 %), Montmorillonite (51.11 %)
FerberiteFeWO473.33%Anthoinite (73.33 %)
BaryteBaSO472.63%Baileychlore (52.63 %), Ranciéite (51.44 %), Takanelite (60.00 %)
ArsenopyriteFeAsS66.66%Malayaite (66.67 %)
PyrrhotiteFe1-xS64.28%Malayaite (64.29 %)
AzuriteCu3(CO3)2(OH)260.98%Rosasite (60.99 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)659.34%Rosasite (59.34 %)
AnglesitePbSO454.02%Rosasite (54.03 %)
DolomiteCaMg(CO3)252.63%Baileychlore (52.63 %)
GypsumCaSO4 · 2H2O52.63%Baileychlore (52.63 %)
BerylBe3Al2(Si6O18)51.21%Bavenite (51.21 %)
GoldAu42.38%Aikinite (52.99 %)

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

Unique: Stolzite, Wulfenite
200
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Mpororoite
143
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Malayaite
133
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Aikinite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)32
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]26
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]16
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)14
34 : Complex granite pegmatites13
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits13
26 : Hadean detrital minerals11
19 : Granitic intrusive rocks7
6 : Secondary asteroid phases7
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)6