Mineral Evolution Database
Created and maintained by the Mineral Evolution Project in partnership with RRUFF and mindat.
Mineral locality data provided by mindat.org

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The goal of this page is to present localities at which the mineral is found, and estimates of the oldest possible geologic age of the minerals at these localities.


Locality Name:
Yunta, Olary Province, South Australia, Australia

Oldest recorded age at locality: 2500
Youngest recorded age at locality: 0

mindat Locality ID: 206490
mindat URL: http://www.mindat.org/loc-206490.html

Tectonic Settings:

Total number of sublocalities beneath "Yunta, Olary Province, South Australia, Australia": 3
Total number of bottom-level sublocalities: 3

Number of Child Localities: 3
Child Localities:
Paratoo Copper Mine
Road Metal Quarry
Robertson Mine

Latitude: 32°40'39"S
Longitude: 139°19'49"E
Decimal Degree (lat, lon): -32.6775,139.33027777778

AThis mineral is Anthropogenic.
GThis mineral is directly dated.
BThis mineral is reported as having this age.
YThis mineral is using an age reported as an element mineralization period.
OThis mineral is using an age calculated from all data at the locality.
RThe age displayed for this mineral originates from a different, non-child locality.
PThe age displayed for this mineral is the range of ages for this mineral at all of this locality's children.
This mineral's age has not yet been recorded.

This Mineral list contains entries from this locality, including sub-localities. Minerals in bold are reported by mindat.org as occurring directly at this locality, and do not occur at any children (sublocalities) of this locality.

Elements at this locality, including sub-localities: Al Ba C Ca Ce Cl Cu Er F Fe H K La Mg Na Nd O P S Si Sr Ti U Y Yb 

Elements from minerals reported directly at this locality: 

Structural Groups for minerals in this locality: 
AllophaneAmphiboleAnalcimeAncyliteApatiteAtacamiteBaryteBastnäsiteBranneriteCalcite
CarbocernaiteChabaziteChalcopyriteClayClinozoisiteConnelliteCorundumDiasporeDigeniteEpidote
FeldsparFluoriteFornaciteGypsumKaoliniteMalachiteMckelveyiteMicaMonaziteNone
Not in a structural groupPyriteQuartzSmectite-vermiculiteSpinelTengeriteTitaniteZircon

50 IMA Minerals at location:
Actinolite  (*)Albite  (*)Analcime  (*)Anorthite  (*)Atacamite  (*)
Azurite  (*)Baryte  (*)Bastnäsite-(Ce)  (*)Bastnäsite-(La)  (*)Brannerite  (*)
Britholite-(Ce)  (*)Calcioancylite-(Nd)  (*)Calcite  (*)Caysichite-(Y)  (*)Celestine  (*)
Chabazite-Na  (*)Chalcopyrite  (*)Chrysocolla  (*)Coffinite  (*)Connellite  (*)
Cuprite  (*)Decrespignyite-(Y)  (*)Digenite  (*)Dolomite  (*)Donnayite-(Y)  (*)
Epidote  (*)Goethite  (*)Gypsum  (*)Hematite  (*)Ilmenite  (*)
Kamphaugite-(Y)  (*)Kaolinite  (*)Magnetite  (*)Malachite  (*)Monazite-(Ce)  (*)
Muscovite  (*)Nontronite  (*)Paratooite-(La)  (*)Pseudomalachite  (*)Pyrite  (*)
Quartz  (*)Siderite  (*)Synchysite-(Ce)  (*)Tengerite-(Y)  (*)Tenorite  (*)
Titanite  (*)Törnebohmite-(La)  (*)Uraninite  (*)Xenotime-(Y)  (*)Zoisite  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Actinolite  (*)Amphibole   Ca2(Mg4.5-2.5Fe2+0.5-2.5)Si8O22(OH)2250001126703419
Albite  (*)FeldsparNa(AlSi3O8)25003.1212670,126718803
Analcime  (*)AnalcimeNa(AlSi2O6)·H2O250001126701627
Anorthite  (*)FeldsparCa(Al2Si2O8)250001126701036
Atacamite  (*)AtacamiteCu2Cl(OH)325000112670544
Azurite  (*)Not in a structural groupCu3(CO3)2(OH)2250001126705509
Baryte  (*)BaryteBa(SO4)2500011267011547
Bastnäsite-(Ce)  (*)BastnäsiteCe(CO3)F5140112670304
Bastnäsite-(La)  (*)BastnäsiteLa(CO3)F514011267030
Brannerite  (*)BranneriteUTi2O625000112670248
Britholite-(Ce)  (*)Apatite(Ce,Ca)5(SiO4)3(OH)5140112670115
Calcioancylite-(Nd)  (*)AncyliteNd2.8Ca1.2(CO3)4(OH)3·H2O51401126705
Calcite  (*)CalciteCa(CO3)2500011267027770
Caysichite-(Y)  (*)None(Ca,Yb,Er)4Y4(Si8O20)(CO3)6(OH)·7H2O51401126708
Celestine  (*)BaryteSr(SO4)250001126701252
Chabazite-Na  (*)Chabazite(Na3K)[Al4Si8O24]·11H2O2500011267066
Chalcopyrite  (*)ChalcopyriteCuFeS22500011267027198
Chrysocolla  (*)Allophane(Cu2-xAlx)H2-xSi2O5(OH)4·nH2O250001126703531
Coffinite  (*)ZirconU(SiO4)·nH2O25000112670566
Connellite  (*)ConnelliteCu36(SO4)(OH)62Cl8·6H2O25000112670295
Cuprite  (*)Not in a structural groupCu2O250001126702970
Decrespignyite-(Y)  (*)NoneY4Cu(CO3)4Cl(OH)5·2H2O51401126701
Digenite  (*)DigeniteCu1.8S250001126701027
Dolomite  (*)NoneCaMg(CO3)2250001126709895
Donnayite-(Y)  (*)MckelveyiteNaSr3CaY(CO3)6·3H2O514011267013
Epidote  (*)Epidote ClinozoisiteCa2(Al2Fe3+)[Si2O7][SiO4]O(OH)25003.1212670,126718173
Goethite  (*)DiasporeFeO(OH)250001126707437
Gypsum  (*)GypsumCa(SO4)·2H2O250001126706890
Hematite  (*)CorundumFe2O32500011267014640
Ilmenite  (*)CorundumFe2+Ti4+O3250001126705433
Kamphaugite-(Y)  (*)NoneCaY(CO3)2(OH)·H2O514011267028
Kaolinite  (*)Clay KaoliniteAl2Si2O5(OH)4250001126705591
Magnetite  (*)SpinelFe2+Fe3+2O42500011267014899
Malachite  (*)MalachiteCu2(CO3)(OH)22500011267012537
Monazite-(Ce)  (*)MonaziteCe(PO4)5140112670945
Muscovite  (*)Mica ClayKAl2(Si3Al)O10(OH)22500011267017380
Nontronite  (*)Clay Smectite-vermiculiteNa0.3Fe3+2(Si,Al)4O10(OH)2·nH2O25000112670471
Paratooite-(La)  (*)Carbocernaite(La,Ca,Na,Sr)6Cu(CO3)851401126701
Pseudomalachite  (*)NoneCu5(PO4)2(OH)425000112670369
Pyrite  (*)PyriteFeS22500011267039462
Quartz  (*)QuartzSiO22500011267061156
Siderite  (*)CalciteFe(CO3)250001126706417
Synchysite-(Ce)  (*)NoneCaCe(CO3)2F5140112670232
Tengerite-(Y)  (*)TengeriteY2(CO3)3·2-3H2O514011267024
Tenorite  (*)NoneCuO250001126701101
Titanite  (*)TitaniteCaTi(SiO4)O253.11126714899
Törnebohmite-(La)  (*)FornaciteLa2Al(SiO4)2(OH)51401126702
Uraninite  (*)FluoriteUO2250001126702718
Xenotime-(Y)  (*)ZirconY(PO4)5140112670939
Zoisite  (*)EpidoteCa2Al3[Si2O7][SiO4]O(OH)250001126701025



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Giersdorf_00000993Uranium mineralization in the Lake Frome area are hosted by paleovalleys and paleochannels which typically run north-south in the Eyre Formation.
Giersdorf_00000993bUranium mineralization in the Lake Frome area are hosted by paleovalleys and paleochannels which typically run north-south in the Eyre Formation.
Michelle_496The Paratoo deposit is hosted in the dolomitic shales of the Burra Formation, near the Adelaidean Paratoo Diapir. A unique REE mineral assemblage is found in the top 2-3 m of the deposit.
Michelle_497The Paratoo deposit is hosted in the dolomitic shales of the Burra Formation, near the Adelaidean Paratoo Diapir. A unique REE mineral assemblage is found in the top 2-3 m of the deposit.


5 Ages assigned to this locality:

Excel IDMax Age (Ma)Min Age (Ma)Age as listed in referenceDating MethodAge InterpretPrioritized?Sample SourceSample NumRun NumAge from other LocalityDated MineralMinerals explicitely stated as having this ageAge applies to these ElementsMinDat Locality IDDated Locality (Max Age)Location as listed in referenceReferenceReference DOIReference IDAge Notes
Giersdorf_00000993252525-4     Yes U159060Northeast, South Australia, AustraliaLake Frome AreaJaireth et al. (2010) AN97_21 
Giersdorf_00000993b646-4     Yes U159060Northeast, South Australia, AustraliaLake Frome AreaJaireth et al. (2010) AN97_21 
Giersdorf_000009945.33.15.3-3.1U-Pb coffinite, carnotite  Yes U159060Northeast, South Australia, AustraliaLake Frome AreaJaireth et al. (2010) AN97_21 
Michelle_4962500252Proterozoic, Paleozoic Age of system activity at deposit      6989Paratoo Copper Mine, Yunta, Olary Province, South Australia, AustraliaParatoo Copper MineBrugger et al. (2006)10.1180/0026461067060361MM70_609Age of system activity at deposit. The precise timing is unknown of the mineralization due to the complex geology. It is estimated that regional activities continued to supply heat, fluids and elements from the Proterozoic to the Paleozoic. The REE minerals were likely very late stage, mineralized with basinal brines, with REE supplied from either the Callana group or Paleo-Mesoproterozoic basement gneisses.
Michelle_4975140Delamerian, 0 Age of youngest deformation     La, Ce, Y, Nd6989Paratoo Copper Mine, Yunta, Olary Province, South Australia, AustraliaParatoo Copper MineBrugger et al. (2006)10.1180/0026461067060361MM70_609Age of Delamerian Orogeny (514 - 500 ma) to recent. The precise age of REE mineralization is unkown due to the complex geology but is likely to be more recent than the Delamerian. It is estimated that regional activities continued to supply heat, fluids and elements from the Proterozoic to the Paleozoic. The REE minerals were likely very late stage, mineralized with basinal brines, with REE supplied from either the Callana group or Paleo-Mesoproterozoic basement gneisses. Sedimentation ceased at the onset of the Delamerian Orogeny.


SampleSource LocalityReference URL
R060302Paratoo Copper Mine, Yunta, Olary Province, South Australia, Australiahttps://rruff.info/R060302
R110066Paratoo Copper Mine, Yunta, Olary Province, South Australia, Australiahttps://rruff.info/R110066


All locality data graciously provided by mindat.org

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