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Predictive Mineralogy

Possible unrecorded species at Eyre Peninsula, South Australia, 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
BerauniteFe3+6(PO4)4O(OH)4 · 6H2O100.00%Bermanite (59.68 %), Jahnsite-(CaMnMn) (100.00 %), Kidwellite (60.00 %), Metaswitzerite (73.08 %), Paravauxite (100.00 %), Robertsite (50.00 %)
RockbridgeiteFe2+Fe3+4(PO4)3(OH)599.98%Bermanite (67.74 %), Hureaulite (51.43 %), Jahnsite-(CaMnMn) (76.00 %), Kidwellite (55.00 %), Metaswitzerite (61.54 %), Mitridatite (51.66 %), Paravauxite (80.95 %), Phosphosiderite (52.13 %), Robertsite (54.55 %)
VivianiteFe2+Fe2+2(PO4)2 · 8H2O99.95%Bermanite (51.61 %), Fairfieldite (58.02 %), Jahnsite-(CaMnMn) (80.00 %), Metaswitzerite (76.92 %), Mitridatite (53.64 %), Paravauxite (80.95 %), Triploidite (50.00 %)
SchorlNaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)99.87%Eosphorite (57.52 %), Fairfieldite (70.37 %), Hureaulite (50.00 %), Jahnsite-(CaMnMn) (64.00 %), Paravauxite (57.14 %), Robertsite (59.09 %), Triploidite (68.75 %)
StrunziteMn2+Fe3+2(PO4)2(OH)2 · 6H2O97.89%Bermanite (50.00 %), Jahnsite-(CaMnMn) (68.00 %), Metaswitzerite (53.85 %), Paravauxite (71.43 %)
LaueiteMn2+Fe3+2(PO4)2(OH)2 · 8H2O97.19%Bermanite (51.61 %), Jahnsite-(CaMnMn) (64.00 %), Metaswitzerite (57.69 %), Paravauxite (61.90 %)
AlmandineFe2+3Al2(SiO4)397.01%Fairfieldite (54.32 %), Jahnsite-(CaMnMn) (64.00 %), Metaswitzerite (57.69 %), Paravauxite (57.14 %)
StewartiteMn2+Fe3+2(PO4)2(OH)2 · 8H2O91.70%Bermanite (51.61 %), Jahnsite-(CaMnMn) (64.00 %), Paravauxite (52.38 %)
FrondeliteMn2+Fe3+4(PO4)3(OH)590.57%Jahnsite-(CaMnMn) (56.00 %), Paravauxite (57.14 %), Robertsite (50.00 %)
Heterosite(Fe3+,Mn3+)PO489.52%Jahnsite-(CaMnMn) (56.00 %), Paravauxite (52.38 %), Robertsite (50.00 %)
TephroiteMn2+2SiO488.70%Pennantite (54.84 %), Pyrosmalite-(Mn) (50.00 %), Sussexite (50.00 %)
FluoriteCaF284.61%Weberite (84.62 %)
BerzelianiteCu2-xSe (x ≈ 0.12)83.67%Eucairite (54.84 %), Umangite (63.86 %)
KlockmanniteCuSe82.99%Eucairite (59.68 %), Umangite (57.83 %)
CacoxeniteFe3+24AlO6(PO4)17(OH)12 · 75H2O80.95%Kidwellite (60.00 %), Paravauxite (52.38 %)
SarkiniteMn2+2(AsO4)(OH)80.00%Arsenoclasite (80.00 %)
BerylBe3Al2(Si6O18)79.99%Bermanite (79.03 %), Eosphorite (71.90 %), Fairfieldite (77.78 %), Hureaulite (71.43 %), Jahnsite-(CaMnMn) (76.00 %), Metaswitzerite (61.54 %), Mitridatite (54.30 %), Paravauxite (66.67 %), Robertsite (68.18 %), Triploidite (68.75 %)
TriphyliteLiFe2+PO479.93%Bermanite (54.84 %), Fairfieldite (66.67 %), Hureaulite (53.57 %), Jahnsite-(CaMnMn) (60.00 %), Metaswitzerite (57.69 %), Paravauxite (66.67 %), Robertsite (59.09 %), Triploidite (53.13 %)
TorberniteCu(UO2)2(PO4)2 · 12H2O77.14%Jahnsite-(CaMnMn) (52.00 %), Paravauxite (52.38 %)
SpessartineMn2+3Al2(SiO4)370.58%Pyrosmalite-(Mn) (70.59 %)
CryoliteNa2NaAlF669.23%Weberite (69.23 %)
ProsopiteCaAl2F4[(OH)4-xFx]69.23%Weberite (69.23 %)
Hydrokenoralstonite Na0.5(Al,Mg)2(F,OH)6 · H2O 69.23%Weberite (69.23 %)
PyrochroiteMn(OH)266.66%Allactite (66.67 %)
Jahnsite-(CaMnFe){Ca}{Mn2+}{Fe2+2}{Fe3+2}(PO4)4(OH)2 · 8H2O64.00%Jahnsite-(CaMnMn) (64.00 %)
PhosgenitePb2CO3Cl263.79%Laurionite (63.79 %)
PyroxmangiteMn2+SiO361.76%Pyrosmalite-(Mn) (61.76 %)
SwitzeriteMn2+3(PO4)2 · 7H2O61.53%Metaswitzerite (61.54 %)
GearksutiteCa[Al(F,OH)5(H2O)]61.53%Weberite (61.54 %)
PachnoliteNaCa[AlF6] · H2O61.53%Weberite (61.54 %)
BeudantitePbFe3(AsO4)(SO4)(OH)658.44%Hidalgoite (58.44 %)
ChildreniteFe2+Al(PO4)(OH)2 · H2O57.14%Paravauxite (57.14 %)
HydroxylapatiteCa5(PO4)3(OH)56.00%Jahnsite-(CaMnMn) (56.00 %)
Riebeckite◻[Na2][Fe2+3Fe3+2]Si8O22(OH)253.84%Weberite (53.85 %)
ThomsenoliteNaCa[AlF6] · H2O53.84%Weberite (53.85 %)
AdeliteCaMg(AsO4)(OH)53.33%Allactite (53.33 %)
PrehniteCa2Al2Si3O10(OH)252.21%Pumpellyite-(Mg) (52.21 %)
EulytineBi4(SiO4)351.85%Namibite (51.85 %)
HydrocerussitePb3(CO3)2(OH)251.72%Laurionite (51.72 %)
ParalaurionitePbCl(OH)51.72%Laurionite (51.72 %)
AnalcimeNa(AlSi2O6) · H2O51.57%Phillipsite-K (51.58 %)
CorkitePbFe3(PO4)(SO4)(OH)650.98%Kintoreite (50.98 %)
ScoroditeFe3+AsO4 · 2H2O50.64%Hidalgoite (50.65 %)
WulfenitePb(MoO4)50.13%Vanadinite (50.14 %)
SulphurS850.00%Sassolite (50.00 %)
CassiteriteSnO241.48%Fairfieldite (51.85 %)

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: Bohdanowiczite, Clausthalite, Crednerite, Eucairite, Guanajuatite, Jalpaite, etc.
896
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Allactite, Hausmannite, Hetaerolite, Kutnohorite, Pennantite, Pyrosmalite-(Mn), etc.
648
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Fraipontite, Halloysite
422
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)

Unique: Arsenoclasite, Gatehouseite, Paravauxite
301
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
284
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite, Iodargyrite
205
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Pseudorutile
137
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Pumpellyite-(Mg)
136
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Sussexite
119
48 : Soil leaching zone minerals

Unique: Gibbsite
117
53 : Other minerals with taphonomic origins

Unique: Middlebackite
114
21 : Chemically precipitated carbonate, phosphate, iron formations

Unique: Montgomeryite
100
34 : Complex granite pegmatites62
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]47
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]47
26 : Hadean detrital minerals41
31 : Thermally altered carbonate, phosphate, and iron formations32
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]22
49 : Oxic cellular biomineralization (see also #44)17
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]17
50 : Coal and/or oil shale minerals16
54 : Coal and other mine fire minerals (see also #51 and #56)15