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Juno Mine ('Peko'; Explorer 8), Tennant Creek, Barkly Region, Northern Territory, Australiai
Regional Level Types
Juno Mine ('Peko'; Explorer 8)Mine
Tennant CreekCreek
Barkly RegionRegion
Northern TerritoryTerritory
AustraliaCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
19° 42' 8'' South , 134° 14' 41'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Tennant Creek3,889 (2012)8.1km
Mindat Locality ID:
125
Long-form identifier:
mindat:1:2:125:1
GUID (UUID V4):
ce06621b-6936-4354-b334-dab44e0961ef


A major gold-copper-bismuth mine closed during November, 1981.
Owned by Gecko. Hosted by ironstones.

The mine hosts three type locality species, being junoite, pekoite, and proudite. Location wise, the first two are uncommon, and the proudite is rare. The species belong to lead and bismuth seleniferous sulphosalts, rarely found in sulphide deposits, and in the past often poorly defined as individual species.

Specimens will often be labelled Juno Mine (Peko) however, it should be noted that Juno and Peko are separate mines, about 2 kilometres apart. The Pekoite species type locality is the Juno mine, it is assumed the name comes from the company (Peko-Wallsend) that mined both deposits. In turn, 'Peko' for the original deposit, is named after a dog.

The original sources describing the type locality material, obtained samples for the mine from outside collections, so shed little light of where the species fit into the overall geology of the mine.

When operational, Juno was the highest grade gold mine in Australia. The Juno lode is vertically zoned with magnetite (80%) and chlorite (20%) forming its core, enclosed by talc-magnetite and minor pyrite, then a thin dolomite zone, and finally chloritised country rock. Gold is concentrated in the core, surrounded by an umbrella shaped bismuth sulphosalt zone, formed by hydrothermal processes at low temperatures. Bismuthinite is concentrated in the basal part of the sulphosalt zone, with chalcopyrite more prevalent in the upper parts. The whole deposit is part of an anticline.

Proudite is named after John S. Proud (1907-1997), a director of the Peko-Wallsend Mining Company. It was initially mis-identified as wittite, due to the rarity of the species, and poorly defined chemical studies on it. Shortly after it was proved to be a new species, and named proudite. It contains 6.5-15.3% Se. The specimen studied came from the University of New England collection. Pekoite is composed of two slabs of bismuthinite and one of krupkaite as ribbons alternating along the B axis as a three fold superstructure. Junoite is up to 11.4% Se.

The deposit before the mine was created was called Explorer 8. Three drill holes had produced negative results in 1954, from what was otherwise a very promising magnetic anomaly. John Elliston purchased the lease for 50 pounds, and continued drilling uncovering the rich but small deposit in 1965. Production commenced in 1968, achieving 838 941 ounces of gold from 346 235 tonnes of ore at 73 g/t, with minor bismuth, silver, and selenium. Peko-Wallsend (Geopeko) operated the mine, along with several rich mines in the area at the time. Ted Davies was area manager, known as Terrible Ted, for terrorising younger less experienced staff.

The underground mine contained a head frame, small processing plant, a few demountable buildings and nearby caravan park for workers. The mine closed in 1981. Several exploration companies have conducted near surface drilling to examine the potential of an open cut mine. The mine site is about 2 kilometres south-west of the Peko mine, or 8 kilometres south-east of Tennant Creek. Little appears to remain at the site apart from some cleared areas and building foundations. The former workman's camp on the road into the mine, is now a public camp site.


Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


23 valid minerals. 3 (TL) - type locality of valid minerals.

Detailed Mineral List:

Aikinite
Formula: PbCuBiS3
Bismuth
Formula: Bi
Bismuthinite
Formula: Bi2S3
Calcite
Formula: CaCO3
Chalcopyrite
Formula: CuFeS2
'Chlorite Group'
Dolomite
Formula: CaMg(CO3)2
Emplectite
Formula: CuBiS2
Gladite
Formula: PbCuBi5S9
Gold
Formula: Au
Guanajuatite
Formula: Bi2Se3
Hematite
Formula: Fe2O3
Heyrovskýite
Formula: Pb6Bi2S9
Description: Selenian variety.
Junoite (TL)
Formula: Cu2Pb3Bi8(S,Se)16
Type Locality:
Krupkaite
Formula: PbCuBi3S6
Magnetite
Formula: Fe2+Fe3+2O4
Matildite
Formula: AgBiS2
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Pekoite (TL)
Formula: PbCuBi11S18
Type Locality:
Proudite (TL)
Formula: CuPb7.5Bi9.33(S,Se)22
Type Locality:
Pyrite
Formula: FeS2
Pyrrhotite
Formula: Fe1-xS
Quartz
Formula: SiO2
Talc
Formula: Mg3Si4O10(OH)2
'Wittite'
Formula: Pb9Bi12(S,Se)27

Gallery:

Cu2Pb3Bi8(S,Se)16 Junoite (TL)

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
Bismuth1.CA.05Bi
Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pyrrhotite2.CC.10Fe1-xS
Bismuthinite2.DB.05Bi2S3
Guanajuatite2.DB.05Bi2Se3
Pyrite2.EB.05aFeS2
Emplectite2.HA.05CuBiS2
Aikinite2.HB.05aPbCuBiS3
Gladite2.HB.05aPbCuBi5S9
Pekoite (TL)2.HB.05aPbCuBi11S18
Krupkaite2.HB.05aPbCuBi3S6
Matildite2.JA.20AgBiS2
'Wittite'2.JB.20Pb9Bi12(S,Se)27
Junoite (TL)2.JB.25aCu2Pb3Bi8(S,Se)16
Proudite (TL)2.JB.25dCuPb7.5Bi9.33(S,Se)22
Heyrovskýite2.JB.40bPb6Bi2S9
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Dolomite5.AB.10CaMg(CO3)2
Group 9 - Silicates
Talc9.EC.05Mg3Si4O10(OH)2
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
'Chlorite Group'-

List of minerals for each chemical element

HHydrogen
H MuscoviteKAl2(AlSi3O10)(OH)2
H TalcMg3Si4O10(OH)2
CCarbon
C CalciteCaCO3
C DolomiteCaMg(CO3)2
OOxygen
O CalciteCaCO3
O DolomiteCaMg(CO3)2
O HematiteFe2O3
O MagnetiteFe2+Fe23+O4
O MuscoviteKAl2(AlSi3O10)(OH)2
O QuartzSiO2
O TalcMg3Si4O10(OH)2
MgMagnesium
Mg DolomiteCaMg(CO3)2
Mg TalcMg3Si4O10(OH)2
AlAluminium
Al MuscoviteKAl2(AlSi3O10)(OH)2
SiSilicon
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si QuartzSiO2
Si TalcMg3Si4O10(OH)2
SSulfur
S AikinitePbCuBiS3
S BismuthiniteBi2S3
S ChalcopyriteCuFeS2
S EmplectiteCuBiS2
S GladitePbCuBi5S9
S JunoiteCu2Pb3Bi8(S,Se)16
S KrupkaitePbCuBi3S6
S MatilditeAgBiS2
S PekoitePbCuBi11S18
S ProuditeCuPb7.5Bi9.33(S,Se)22
S PyriteFeS2
S PyrrhotiteFe1-xS
S WittitePb9Bi12(S,Se)27
S HeyrovskýitePb6Bi2S9
KPotassium
K MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Ca CalciteCaCO3
Ca DolomiteCaMg(CO3)2
FeIron
Fe ChalcopyriteCuFeS2
Fe HematiteFe2O3
Fe MagnetiteFe2+Fe23+O4
Fe PyriteFeS2
Fe PyrrhotiteFe1-xS
CuCopper
Cu AikinitePbCuBiS3
Cu ChalcopyriteCuFeS2
Cu EmplectiteCuBiS2
Cu GladitePbCuBi5S9
Cu JunoiteCu2Pb3Bi8(S,Se)16
Cu KrupkaitePbCuBi3S6
Cu PekoitePbCuBi11S18
Cu ProuditeCuPb7.5Bi9.33(S,Se)22
SeSelenium
Se GuanajuatiteBi2Se3
Se JunoiteCu2Pb3Bi8(S,Se)16
Se ProuditeCuPb7.5Bi9.33(S,Se)22
Se WittitePb9Bi12(S,Se)27
AgSilver
Ag MatilditeAgBiS2
AuGold
Au GoldAu
PbLead
Pb AikinitePbCuBiS3
Pb GladitePbCuBi5S9
Pb JunoiteCu2Pb3Bi8(S,Se)16
Pb KrupkaitePbCuBi3S6
Pb PekoitePbCuBi11S18
Pb ProuditeCuPb7.5Bi9.33(S,Se)22
Pb WittitePb9Bi12(S,Se)27
Pb HeyrovskýitePb6Bi2S9
BiBismuth
Bi AikinitePbCuBiS3
Bi BismuthBi
Bi BismuthiniteBi2S3
Bi EmplectiteCuBiS2
Bi GladitePbCuBi5S9
Bi GuanajuatiteBi2Se3
Bi JunoiteCu2Pb3Bi8(S,Se)16
Bi KrupkaitePbCuBi3S6
Bi MatilditeAgBiS2
Bi PekoitePbCuBi11S18
Bi ProuditeCuPb7.5Bi9.33(S,Se)22
Bi WittitePb9Bi12(S,Se)27
Bi HeyrovskýitePb6Bi2S9

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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