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It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Redeemer Gold Mine, Agnew Goldfield (Lawlers), Leonora Shire, Western Australia, Australiai
Regional Level Types
Redeemer Gold MineMine
Agnew Goldfield (Lawlers)Ore Field
Leonora ShireShire
Western AustraliaState
AustraliaCountry

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Latitude & Longitude (WGS84):
28° 3' 41'' South , 120° 28' 59'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
240064
Long-form identifier:
mindat:1:2:240064:1
GUID (UUID V4):
0


The Redeemer Gold Mine is 8 kilometres south south-west of the Agnew Hotel. The deposit was discovered by Western Mining Corporation in 1985. The open pit is presently being infilled by waste rock from other mines.

Production from 1988 to 2002 totalled 11.31 Mt at 3.89 g/t yielding 1.411 million ounces. Open pit mining from 1988 to 1991 achieved 2.09 Mt at 3.53 g/t yielding 0.238 million ounces. Underground mining from 1990 to 2002 achieved 9.2 Mt at 3.97 g/t yielding 1.176 million ounces. A resource remains of 3.16 Mt at 4.4 g/t.

The deposit is found on the Emu Shear Zone. It lies beneath a lag strewn surface of saprolite, tillite and gravel, and is gold poor.

The lower stratabound mineralisation is hosted by the mafic conglomerate unit near the base of the Scotty Creek Formation. Five zones of mineralisation have been defined:

1) Redeemer Main : This is the major ore source, containing poor veining and sulphides, but abundant biotite and actinolite alteration. The gold occurs as fine grains interstitial to coarse actinolite and biotite. A number of (un-named) Bi-Te sulphides, chalcopyrite, molybdenite and scheelite occurs in the ore zone which grades at 4 to 5 g/t.

2) West Lode: Has similar geology to Redeemer Main with less intense biotite alteration, and has numerous quartz-carbonate veins through the mafic conglomerate.

3) North Pipe: A high grade shoot located east of the Redeemer Fault and West Lode, on the Hanging wall between the mafic and ultramafic conglomerate. Gold is associated with quartz-carbonate veins and coarse arsenopyrite.

4 & 5) Zones 2 and 3: These are more typical small quartz vein zones, found in intermediate conglomerate to the west of the Redeemer Main, with weak biotite-actinolite alteration and coarse arsenopyrite.



Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


12 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Actinolite
Formula: ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Arsenopyrite
Formula: FeAsS
'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Chalcopyrite
Formula: CuFeS2
Ilmenite
Formula: Fe2+TiO3
Molybdenite
Formula: MoS2
Native Gold
Formula: Au
Pyrrhotite
Formula: Fe1-xS
Quartz
Formula: SiO2
Rutile
Formula: TiO2
Scheelite
Formula: Ca(WO4)
Talc
Formula: Mg3Si4O10(OH)2
Tremolite
Formula: ◻Ca2Mg5(Si8O22)(OH)2

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pyrrhotite2.CC.10Fe1-xS
Molybdenite2.EA.30MoS2
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
Ilmenite4.CB.05Fe2+TiO3
Quartz4.DA.05SiO2
Rutile4.DB.05TiO2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Scheelite7.GA.05Ca(WO4)
Group 9 - Silicates
Actinolite9.DE.10◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Tremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2
Talc9.EC.05Mg3Si4O10(OH)2
Unclassified
'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2

List of minerals for each chemical element

HHydrogen
H Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
H BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
H TalcMg3Si4O10(OH)2
H Tremolite◻Ca2Mg5(Si8O22)(OH)2
OOxygen
O Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
O BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
O IlmeniteFe2+TiO3
O QuartzSiO2
O RutileTiO2
O ScheeliteCa(WO4)
O TalcMg3Si4O10(OH)2
O Tremolite◻Ca2Mg5(Si8O22)(OH)2
FFluorine
F BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MgMagnesium
Mg Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Mg BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mg TalcMg3Si4O10(OH)2
Mg Tremolite◻Ca2Mg5(Si8O22)(OH)2
AlAluminium
Al BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
SiSilicon
Si Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Si BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Si QuartzSiO2
Si TalcMg3Si4O10(OH)2
Si Tremolite◻Ca2Mg5(Si8O22)(OH)2
SSulfur
S ArsenopyriteFeAsS
S ChalcopyriteCuFeS2
S MolybdeniteMoS2
S PyrrhotiteFe1-xS
KPotassium
K BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
CaCalcium
Ca Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Ca ScheeliteCa(WO4)
Ca Tremolite◻Ca2Mg5(Si8O22)(OH)2
TiTitanium
Ti BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Ti IlmeniteFe2+TiO3
Ti RutileTiO2
FeIron
Fe Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Fe ArsenopyriteFeAsS
Fe BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fe ChalcopyriteCuFeS2
Fe IlmeniteFe2+TiO3
Fe PyrrhotiteFe1-xS
CuCopper
Cu ChalcopyriteCuFeS2
AsArsenic
As ArsenopyriteFeAsS
MoMolybdenum
Mo MolybdeniteMoS2
WTungsten
W ScheeliteCa(WO4)
AuGold
Au Native GoldAu

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

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