Moyagee Project- WA (Silver Lake 100%)

Background

Silver Lake’s Moyagee project has been the subject of several phases of exploration since the early 1980s. Past gold production from the project area totalled 11,780 oz from some 9,400 tonnes of ore mainly from small high grade quartz veins.

Location

Figure 1Figure 1
Moyagee location planClick image to enlarge

The Moyagee project is located within the Archaean Mount Magnet-Meekatharra greenstone belt in the Murchison Province of the Yilgarn Block of Western Australia. It lies between the towns of Mount Magnet and Cue, 600 km northeast of Perth. The project consists of six granted tenements covering 60 km2 with another 250 km2 under application. The Lena prospect and all historical workings lie within granted tenements. 

Geology

The project covers mafic to ultramafic intrusive and volcanic rocks of the north-northeast trending Gabanintha and Golconda Formations, which are truncated in the south by the regional Cuddingwarra Shear. The northeast trending Lena Shear, which is a splay off the Cuddingwarra Shear, is the principal host to the known gold mineralisation within the project area. The trace of the Lena Shear under lacustrine sediments of Lake Austin through Silver Lake’s project area has recently been defined by scout exploration drilling and aeromagnetic imaging.

The ultramafic dominated Lower Gabanintha Formation has generally been considered an unfavourable host for gold mineralisation in this part of the Murchison Province. Tholeiitic basalts and dolerites of the overlying Upper Gabanintha Formation are host to over 50% of the known gold mineralisation within the Murchison Province including the 2Moz Great Fingall mining centre near Cue, 30 km north of Moyagee. The Lena Shear transgresses this greenstone stratigraphy at a low angle with good potential to cut the prospective Upper Gabanintha Formation in the northern portion of Silver Lake’s project area.

Resources

 

 Measured Resources Indicated Resources Inferred Resouces Total Resources 
Deposit Ore
t
'000s 
Grade
g/t
Au 
Total
Oz Au
'000s 
Ore
t
'000s 
Grade
g/t
Au  
Total
Oz Au
'000s  
Ore
t
'000s 
Grade
g/t
Au  
Total
Oz Au
'000s  
Ore
t
'000s 
Grade
g/t
Au  
Total
Oz Au
'000s
  
Moyagee  -  820.2 8.5 224.2820.28.5 224.2 

The gold mineralisation is associated with gold-bearing quartz veins contained within the near-vertical Lena Shear (refer to Figure 2). The resource is located in an area of shallow cover to the south of Lake Austin.  

The integration of previous RAB and aircore drilling results with recent detailed aeromagnetic imagery has outlined a linear trend of anomalous gold mineralisation that can be traced north-northeast from the sub-cropping Lena resource area. Significantly, this linear trend corresponds to a marked linear aeromagnetic feature interpreted as the Lena Shear.

Previous Drilling Results From Within The Lena Resource
Hole IDFrom (m)To (m)Downhole Interval (m)Gold (g/t)
MGRC 162102107557.3
MGDD 3354.83616.231.4
MGDD 21220222281.3
MGDD 2371.3378.47.116.2
MGDD 9364.9367.9331.2
MGRC 1903334186.7
MORC 0192729241.5
MORC 0095456238.2
MGDD 12367.9372.24.314.4
MGRC 17812313078.4
MGRC 207677478.1
MGRC 0051620414
MGRC 0103741413.9
MGDD 4223.8224.8151.2

Figure 2Figure 2
Geological cross-section through the Lena prospectClick image to enlarge

Exploration Programme

The Lena prospect, at Moyagee, is the primary target for exploration in the coming year. In the second quarter of 2009 a deep diamond drilling programme will commence to test the dip and strike continuity of this resource which remains open at depth and to the north and south. The programme is designed to extend the Lena resource to the north and south by drilling four holes along three separate 60 metres spaced sections. It is also proposed to complete a 650 metres deep diamond drill hole on each of the five existing drill traverses that currently define the Lena resource to test the down dip extent of the deposit.  

Systematic drill testing of the northern portion of Silver Lake’s project area where the Lena Shear transgresses prospective basalts and dolerites of the Upper Gabanintha Formation will also be carried out.  


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