Fuzerradvany Concession


At the Fuzerradvany Concession, rhyolite tuffs and ignimbrite overlie unexposed metamorphosed Paleozoic and Precambrian basement. Sandstones and siltstones overlie the rhyolite units. Late-stage rhyolite intrusives cut the sediments. Geological mapping has defined a large area of hot spring style alteration covering 1.2 km². Alteration features include areas of opaline-chalcedonic silicification related sinters, hydrothermal eruption breccias and pockets of advanced-argillic and argillic alteration.

Three discrete northwest trending Au-in-soil anomalies have been outlined within this area of alteration. The strongest anomaly, with dimensions of 800 m by 60-300 m, has gold values ranging from 15-330 ppb Au. There are coincident arsenic, antimony and mercury anomalies associated with this gold anomaly. Within this anomaly there is a 15 m wide breccia zone cut by banded chalcedonic quartz veins, cherty silicification with stockwork quartz veinlets, and sulphide-bearing grey silicification. Proximal to this anomaly is an underground illite mine, which contains chalcedonic-opaline quartz veinlets. Several channel samples ranged from 1.0 to 1.22 g/t Au with selected grab samples ranging from 0.57 to 13.47 g/t Au.


The geologic features of the Penga Oldal Au-anomaly, including close proximity to an illite deposit, and inclusion within a large area of hydrothermal alteration suggests good potential for an upper-level quartz-adularia Au-Ag deposit or hot springs-type Au-Ag deposit with the potential to host a large precious metal deposit. This target anomaly has similarities with the Kremnica Resource in Slovakia (22.3 Mt at 1.54 g/t Au for 1.1 Moz Au), mainly high-level low sulphidation mineralization related to late-stage rhyolite intrusives, and as such is considered a high quality drill target.

Drilling in late 2007 on (6 core holes for 806 metres) all intersected alteration features consistent with a shallow-level epithermal mineralized system.  Locally, the alteration-mineralization features intersected include hydrothermal breccias, cross-cutting banded quartz-chalcedony veinlets, lattice-structure quartz, and disseminated fine-grained sulphides in intensely silicified tuffs.  Assay results indicate this alteration-mineralization system is gold and silver bearing with 5 of 6 drill holes intersecting discrete zones with > 1.0 g/t Au.  Drill intersections and drill hole descriptions are shown in the tables below and on the accompanying drill plan map.

Drill hole intersections from the Fuzerradvany Concession initial drill program, December 2007.


Drill Hole

From
(m)

To
(m)

Length
(m)

Thickness*
(m)

 Au
(g/t)

Ag
(g/t)

 

 

 

 

 

 

 

FR-55

28

47

19

12

0.63

16

Incl

38

39.3

1.3

0.8

2.49

21

 

83

85

2

1.2

3.23

68

 

119

121

2

1.2

2.09

160

FR-57

101

105

4

2.5

1.03

53

Incl

103

104

1

0.6

3.15

159

 

111

112

1

0.6

5.73

75

 

132

156

24

15

1.7

171

Incl

138

154

16

10

2.35

237

Incl

144

153

9

5.6

3.33

247

FR-61

58.9

60

1.1

0.7

3.16

883

 

66

71

5

3.1

1.22

31

Incl

70

71

1

0.6

4.27

15

FR-68

145

148

3

1.9

1.34

25

FR-69

NSI

 

 

 

 

 

FR-74

28.74

59

30.26

19

0.67

40

Incl

28.74

29.74

1

0.6

2.94

946

 

 

 

 

 

 

 

 

 

 

 

 

 

NSI = no significant intersections
*Estimated true thickness

 

Drill hole details Table from the Fuzerradvany Concession initial drill program, December 2007.

Drill Hole

Fence

Azimuth (degrees)

Declination (degrees)

Total Depth (meters)

FR-74

1000N

260

-52

127.2

FR-68

1000N

260

-50

148.0

FR-69

1000N

80

-47

107.1

FR-55

870N

230

-50

150.1

FR-57

690N

230

-50

160.8

FR-61

550N

230

-50

112.6

Note: all drill holes are diamond core

    


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