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Predictive Mineralogy

Possible unrecorded species at Cloncurry Shire, Queensland, 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
AragoniteCaCO392.49%Hörnesite (57.60 %), Huntite (51.32 %), Spertiniite (63.64 %)
CopiapiteFe2+Fe3+4(SO4)6(OH)2 · 20H2O90.97%Coquimbite (57.89 %), Kornelite (57.14 %), Voltaite (50.00 %)
StrengiteFePO4 · 2H2O83.27%Hentschelite (56.52 %), Natrodufrénite (61.54 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)683.25%Claringbullite (58.82 %), Rosasite (59.34 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O82.82%Torbernite (51.52 %), Uranocircite (64.58 %)
LinaritePbCu(SO4)(OH)282.11%Beaverite-(Cu) (52.10 %), Leadhillite (62.67 %)
TalmessiteCa2Mg(AsO4)2 · 2H2O80.00%Anorthoroselite (60.00 %), Cobaltaustinite (50.00 %)
SkutteruditeCoAs378.88%Anorthoroselite (52.00 %), Roselite (56.00 %)
CornwalliteCu5(AsO4)2(OH)458.21%Clinoclase (58.22 %)
RhodoniteCaMn3Mn[Si5O15]57.98%Bustamite (57.98 %)
ArseniosideriteCa2Fe3+3(AsO4)3O2 · 3H2O57.14%Cobaltaustinite (57.14 %)
ThoriteTh(SiO4)56.66%Stillwellite-(Ce) (70.83 %)
BrauniteMn2+Mn3+6(SiO4)O854.61%Bixbyite-(Mn) (54.62 %)
RhodochrositeMnCO354.54%Alabandite (54.55 %)
BerauniteFe3+6(PO4)4O(OH)4 · 6H2O53.84%Natrodufrénite (53.85 %)
RömeriteFe2+Fe3+2(SO4)4 · 14H2O53.57%Kornelite (53.57 %)
ChalcosideriteCuFe3+6(PO4)4(OH)8 · 4H2O52.17%Hentschelite (52.17 %)
SpionkopiteCu39S2851.06%Geerite (51.06 %)
PetziteAg3AuTe250.89%Sylvanite (50.89 %)
AntimonySb50.00%Costibite (50.00 %)
UranophaneCa(UO2)2(SiO3OH)2 · 5H2O50.00%Phurcalite (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: Allargentum, Boulangerite, Bournonite, Costibite, Dyscrasite, Geerite, etc.
1,663
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Cuprotungstite, Tungstite
581
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
274
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Bixbyite-(Mn), Pyrosmalite-(Fe)
204
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite
140
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]138
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Spherocobaltite
123
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
120
34 : Complex granite pegmatites

Unique: Yttrotantalite-(Y)
116
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Davidite-(La)
111
52 : Guano- and urine-derived minerals

Unique: Nitromagnesite
105
36 : Carbonatites, kimberlites, and related igneous rocks

Unique: Bastnäsite-(La)
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)57
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]55
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]43
50 : Coal and/or oil shale minerals39
56 : Slag and smelter minerals (see also #51 and #55)39
6 : Secondary asteroid phases37
53 : Other minerals with taphonomic origins37
54 : Coal and other mine fire minerals (see also #51 and #56)35
26 : Hadean detrital minerals32