torre1

SEARCH

  • Default
  • Title
  • Date
  • Random

Shopping Cart

0 item(s) - R0.00
Your shopping cart is empty!
Welcome visitor you can login or create an account.

Zn 0.75% SEDEX Kihabe BW

Category: BASE METALS 
Product Code: AMIS 0082

Available Options


* Select Package Size:














Qty:  

DOWNLOAD AMIS CERTIFICATE (PDF)
AMIS0082 Zinc and Lead, SEDEX, 0.7 & 0.3%, Botswana

Normal 0 false false false MicrosoftInternetExplorer4 

Origin of material: This material was provided by Mt Burgess Mining (NL) from their Kihabe Base Metals Project is located on the border of Botswana and Namibia about 700km north-west of the capital, Gaborone, in Ngamiland. The Project is 350km by road from Maun and 50km from Tsumkwe, Namibia. The target is within a Proterozoic belt of metasedimentary rocks, with around one third of the prospective geology occurring in Botswana (PL 69/2003, area ~1,000km²) and two thirds in Namibia.

The belt of Proterozoic sedimentary rocks, composed primarily of carbonate and siliclastic rocks, form a trapezoidal wedge of tightly to isoclinally folded metamorphosed sediments of the Damaran Supergroup, bounded by granites and gneisses of the Quangwadum Complex and Kihabe Complex. The target mineralisation is primarily stratiform to stratabound sedimentary exhalative (SEDEX) sulphides occurring at a known stratigraphic level within the basin. The Company’s geological model is that the Belt represents a re-closed rift basin with a fill of arkose, greywacke, quartzites and sabkha-facies stromatolitic dolomites.  Mineralisation occurs between dolomite and quartzite for a combined strike length of 450km, within Namibia and Botswana.

The Kihabe Resource is located along a contact between the dolomite footwall and a sequence of rhythmically bedded sandstones, which have been folded and metamorphosed to, respectively, dolomitic marble and chloritic quartzite. The local geology of the deposit is known to be a west-plunging syncline. Mineralisation is developed within the host quartzite within thick, coarse grained beds, and weakens upwards in the stratigraphy as the grain size reduces. Mineralisation forms a series of overlapping stacked horizons controlled by the beds within the quartzite.

Normal 0 false false false MicrosoftInternetExplorer4

Recommended Concentration and two “Between Laboratory” Standard Deviations

 
 

Certified Concentrations

 
 

Zn M/ICP

7520

±

398

ppm

Zn P

7233

±

512

ppm

Zn XRF

7590

±

186

ppm

Pb M/ICP

3089

±

180

ppm

Pb P

3037

±

178

ppm

Cu M/ICP

125

±

10

ppm

Cu P

123

±

10

ppm

Specific Gravity

2.74

±

0.12

 

 
 
 

 

Provisional Concentrations

 
 

Pb XRF

3326

±

480

ppm

Cu XRF

134

±

21.5

ppm

Ag M/ICP

4.7

±

0.7

ppm

 
 
 

 

Indicated Value

 
 

Au Pb Collection

0.02

g/t

 

 

 

 

Normal 0 false false false MicrosoftInternetExplorer4

Major Element Certified Concentrations

 
 

Al2O3

8.68

±

0.26

%

CaO

1.12

±

0.03

%

Fe2O3

3.19

±

0.08

%

K2O

3.23

±

0.08

%

MgO

1.38

±

0.08

%

MnO

0.05

±

0.004

%

P2O5

0.10

±

0.01

%

SiO2

75.98

±

1.82

%

TiO2

0.46

±

0.02

%

S ICP

1.09

±

0.10

%

LOI

2.82

±

0.32

%

 

 

 

Major Element Provisional Concentrations

 
 
 

Cr2O3

0.08

±

0.01

%

Na2O

1.41

±

0.26

%

 

 

PLEASE DOWNLOAD THE CERTIFICATE FOR MORE INFORMATION

 

 

Converter

Untitled Document
From  
To  
gram = 1 gram
Quantity



1

payment

vm

VCS is a Reserve Bank Registered System Operator and a Member of Association of System Operators.