9 March 2021

ASX CODE: MTB

KIHABE POLYMETALLIC DEPOSIT, BOTSWANA

COPPER GRADES NOT CURRENTLY INCLUDED IN THE MINERAL RESOURCE ESTIMATE

Previous Assessment

On 7 September 2020, the Company released an announcement to the ASX, headed 'Kihabe Polymetallic Deposit - Copper Grades not currently Included in the Mineral Resource Estimate'.

This announcement shows that in the NE sector of the Kihabe Deposit, some 15 drill holes intersected potentially commercial copper grades over 600m strike length from section 11,200mE to Section 11,800mE.

In March 2007, Ravensgate, independent geological consultants, compiled an Inferred Mineral Resource estimate (under the 2004 JORC Code) for copper at various low-grade cuts in this NE sector of the Kihabe Deposit (Refer to Table 1).

Because focus on the Kihabe resource at the time only concentrated on Zn/Pb/Ag, none of the additional credits for Vanadium, Germanium and Copper were taken into account.

Recent Assessment

Following increases in the copper price since September 2020, currently in excess of US $8,800/t, the Company has conducted further in-depth assessment of this zone where Cu occurs in association with the Zn/Pb/Ag/Ge/V mineralisation.

This recent assessment has taken into account results from five additional diamond core holes drilled into the area of Cu mineralisation since Ravensgate compiled the Inferred Mineral Resource Estimate (Refer Table 2 and Figure 1). The assessment has shown:

  • This zone of Cu mineralisation now extends from 11,200mE to 12,000mE, covering a potential strike length of 800m.

  • The 17 drill holes now taken into account show that the average width of Cu mineralisation per drill hole amounts to 18.4m

  • The average grade of the mineralised intersections of the 17 drill holes amounts to 0.27% Cu/t.

  • Results from the five additional diamond core holes (highlighted in orange in Table 2) will enable the Company to better understand the continuity of the Cu mineralised zones.

  • Subject to funding, the results from the five additional diamond core holes will enable the Company to more precisely plan future in-fill drilling programmes. Lines of drill holes in this area are mainly 100m apart, which now need to be reduced.

Further Leach Extraction and Mineralogical Test Work

Further leach test work is being conducted to confirm the Zn metal on site recoveries from the Kihabe oxide zone. Mineralogical test work is also being conducted to confirm the host mineral of Vanadium in the Kihabe oxide zone. At the Nxuu Deposit, 7km to the east of the Kihabe Deposit, the host mineral of Vanadium has been confirmed as Descloizite. In Descloizite, Vanadium Pentoxide (V2O5) is 1.785 times the grade of Vanadium (V).

All assay results from drill holes shown in Table 2 have previously been released to ASX.

The Kihabe Deposit with various zones of Zn/Pb/Ag/Cu/Ge/V mineralisation covers an overall strike length of 2,400m and is situated 7km West of the Nxuu Deposit.

The 2004 JORC Code Kihabe Deposit Mineral Resource Statement, showing the Zn equivalent grade for only Zn/Pb/Ag, is attached as Table 3.

Table 1

Mineral Resource Statement - 16 March 2007

(2004 JORC Code) - Kihabe Base Metals

Deposit - Cu Mineralisation - Inferred Resource - Reported at % Cu lower cut-offs

Table 2

HOLE ID

COORDINATES

DIP

AZI-MUTH

INTERVAL

Copper Grade %

Oxide

(O)/ Sulphide

(S)

Easting

Northing

Degrees

Degrees

From (m)

To (m)

Width (m)

Section 11,200E

KRC092

11,200E

10.070N

-60

160

65

67

2

0.18

S

71

73

2

0.13

S

74

76

2

0.13

S

78

83

5

0.14

S

103

105

2

0.42

S

KRC093

11,200E

10,100N

-60

159

100

109

9

0.14

S

123

126

3

0.19

S

Section 11,300E

KRC090

11,300E

10.114N

-60

159

136

146

10

0.16

S

Section 11,450E

KDD140

11,450E

10,100N

-60

339

73

77

4

0.13

S

91

97.50

6.50

0.67

S

Section 11,500E

KDD114

11,500E

10,073N

-90

0

9

54

45

0.16

O

60

63

3

0.13

O

66

68

2

0.39

S

97

99

2

0.94

S

101

104

3

0.15

S

106

117

11

0.37

S

inc

116

117

1

1.44

S

118

128

10

0.43

S

inc

125

126

1

1.22

S

KRC049

11,500E

10,099N

-60

159

28

31

3

0.15

O

32

47

15

0.17

O

50

65

15

0.27

O

KRC052

11,500E

10,129N

-60

159

63

65

2

0.12

O

69

77

8

0.12

S

80

84

4

0.11

S

86

89

3

0.15

S

92

94

2

0.16

S

115

121

6

0.20

S

122

140

18

0.43

S

inc

125

127

2

0.75

S

inc

130

133

3

0.76

S

Section 11,600E

KDD115

11,600E

9,900N

-60

339

38

39

1

0.20

O

50

51

1

0.16

O

119

120

1

0.11

S

151

152

1

0.10

S

181

182

1

0.11

S

KDD143

11,600E

10,010N

-60

339

45

47

2

0.12

O

52

54

2

0.13

O

112

113

1

0.12

S

126

130

4

0.22

S

Table 2 (cont'd)

HOLE ID

COORDINATES

DIP

AZI-MUTH

INTERVAL

Copper Grade %

Oxide

(O)/ Sulphide

(S)

Easting

Northing

Degrees

Degrees

From (m)

To (m)

Width (m)

Section 11,600E

KIH007

11,607E

10,037N

-60

339

62

64

2

0.12

O

95

96

1

2.45

S

98

101

3

0.18

S

135

138

3

0.43

S

inc

136

137

1

1.06

S

KRC056

11,600E

10,110N

-60

159

61

64

3

0.17

O

69

71

2

0.13

O

72

75

3

0.16

S

99

101

2

0.21

S

KRC058

11,595E

10,130N

-60

159

87

91

4

0.24

S

92

95

3

0.52

S

112

115

3

0.19

S

Section 11,700E

KRC072

11,700E

10,150N

-60

159

125

130

5

0.28

S

137

141

4

0.20

S

Section 11,770E

KIH011

11,769E

10,124N

-60

339

54

56

2

0.18

O

60

62

2

0.39

S

63

66

3

0.32

S

71

78

7

1.04

S

81

86

5

0.21

S

87

89

2

0.39

S

Section 11,800E

KRC076

11,800E

10,075N

-60

159

17

37

20

0.28

O

inc

23

25

2

0.71

O

42

47

5

0.31

O

inc

46

47

1

1.34

O

KRC077

11,800E

10,090N

-60

159

37

43

6

0.23

O

Section 12,000E

KDD117

12,000E

11,090N

-60

159

76

78

2

0.23

S

82

86

4

0.19

S

92

93

1

0.29

S

106

110

4

0.22

S

This is an excerpt of the original content. To continue reading it, access the original document here.

Attachments

  • Original document
  • Permalink

Disclaimer

Mount Burgess Mining NL published this content on 09 March 2021 and is solely responsible for the information contained therein. Distributed by Public, unedited and unaltered, on 17 March 2021 05:21:09 UTC.