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Glandore: The Axial Planar Fault |
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The Axial Planar Fault has been intersected by drilling over a strike
length of approximately 400m, to a maximum depth of around 150m below
surface and it is open at depth and along strike in both directions.
Drilling to date suggests that gold has been depleted in the upper
region (approximately 30m of weathered rock) with continuous
mineralised structure beneath. The favourable rock type is the
granophyric zone and mineralisation is known to exist where north west
trending faults intersect this zone. Known mineralisation to date dips
60° to the south west and strikes north west.
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The Axial Planar Fault is some 200m east of the Supergene Zone and
has parallel dip. Numerous intersections show strong grades including 1m at 10.9g/t from 103m, 1.2m at 12.5g/t from 92.5m, 4.8m at 2.84g/t from 81m and 10.25m at 10.3g/t from 58m.
Drilling of the Axial Planar fault is aiming initially to infill the
previous widely spaced holes with the opportunity to test the depth and
strike extension potential in the future.
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Significant Axial Planar Fault Zone drill intercepts (>1.5g/t)
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Drill
Hole
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From
(m)
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Interval
(m)
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Grade
(g/t Au)
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GDJD259
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68.2
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0.6
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6.80
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GDJD260
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90.7
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3.3
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1.97
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GDJD336
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58
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10.25
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10.3
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GDJD339
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103.9
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1.0
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10.9
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GDJD340
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81
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4.8
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2.84
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GDJD341
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105.7
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1.7
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3.3
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GDJD342
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125.8
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2.75
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2.57
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GDJD343
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92.5
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1.2
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12.5
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GDJD344
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54
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6
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1.79
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GDJD345
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62.1
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0.8
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3.89
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GDJD348
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48.4
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1.6
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3.61
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GDJD351
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31.4
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0.6
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2.39
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GDJD353
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167.1
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3.9
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1.23
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GDJD81
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49
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7
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2.61
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88
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10
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1.55
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106
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3
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4.63
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EGRC002
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100
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2
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2.21
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