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RAND MINING LIMITED Interim / Quarterly Report 2012

Dec 10, 2012

65721_rns_2012-12-10_8554ca43-18f4-4e76-a17b-c3c49684b909.pdf

Interim / Quarterly Report

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ACN 139 342 859

11[th] December 2012

Mr Anton Billis,

Director,

Rand Mining Ltd

PO Box 307

West Perth 6872

Dear Anton,

RE: EKJV Exploration Results – September Quarter 2012.

As you requested I have reviewed the Barrick Report “Quarterly Exploration Report: September 2012 EKJV. The Barrick Report is attached and is suitable for release to the market.

Yours sincerely,

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Matthew Sullivan

B.App.Sc, M. Aus.I.M.M

Competency Statement

The information in this report in relation to Exploration Results and Mineral Resources is based on information reviewed by Matthew Sullivan who is a Member of the Australasian Institute of Mining and Metallurgy and has sufficient exploration experience which is relevant to the style of mineralisation under consideration to qualify as a Competent Person as defined in the 2004 Edition of the “Australian Code for Reporting Exploration Results, Mineral Resources and Ore Reserves”. Mr. Sullivan is a full time employee of Jemda Pty Ltd, consultants to Rand Mining and consents to the inclusion of the matters based on this information in the form and context in which it appears.

Office Address: 20 Meelup Way Ridgewood WA 6030

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Quarterly Exploration Report: September 2012 EKJV Quarterly Activity

Summary

This report provides a quarterly report on work conducted by Barrick Kanowna on the East Kundana Joint Venture (EKJV). The EKJV is a joint venture between Barrick Gold subsidiary company Gilt-Edge Mining NL(GEM) and Rand Mining Ltd and Tribune Resources Ltd.

Work was conducted on two prospects within the EKJV on mining lease M16/309. They were:

Pegasus, and

Drake.

At the Pegasus prospect two resource development drill programs were undertaken. These included completing geotechnical and metallurgical drilling and condemnation drilling, as well as resource infill drilling.

At the Drake prospect area a resource development drill program was completed.

Figure 1 shows a collar plan of the September quarter drilling.

Pegasus

The September quarter of 2012 saw a substantial amount of drilling take place at the Pegasus deposit to infill existing drill data in the near surface mineralisation adding to the work completed in the first half of 2012, as well as some mine feasibility work for mine optimisation.

Two drill programmes consisting of 38 drill holes were drilled within the Pegasus project following on from positive outcomes achieved in 2012. Objectives for the drill programmes included the completion of the infill drilling of the high grade core of the Pegasus Open Pit deposit, depth testing of the K2 structure, infilling between the deeper drilling and the optimised pit and the completion of the condemnation programme of an area for the proposed waste dump. Also completed were the drill holes for geotechnical information and metallurgical testing.

Figure 2 shows an updated long projection of the K2 mineralisation for the Pegasus project.

Drilling

A total of 19 diamond drill holes were completed during the quarter for a total advance of 4,697.9m. A total of 19 reverse circulation drill holes were drilled for a total advance of 3,033m.

Results for this are tabled below (Table 1). Significant intersections are listed:

PGCD12017 4.0m @ 46.0 g/t Au from 195.0m and
8.9m @ 10.4 g/t Au from 213.0m
PGDC12018 5.0m @ 25.0 g/t Au from 167.0m
PGCD12047 9.0m @ 5.77 g/t Au from 482.0m
PGDD12059 19.1m @ 8.13 g/t Au from 131.8m
PGDD12060 13.6m @ 16.4 g/t Au from 137.8m
PGRC12064 38.0m @ 7.23 g/t Au from 94.0m
PGDD12096 4.0m @ 12.7 g/t Au from 164.0m
PGDD12110 7.0m @ 5.84 g/t Au from 213.0m
PGDD12116 4.2m @ 9.44 g/t Au from 55.0m

Drake

A small infill drill program was c ompleted at the Dr a ke prosp e ct. The Drake pro s pect is a p proximatel y 200m nor t h along strike from th e Pegasus d eposit on t he same s t ructure.

Drilling

A t otal of 10r e verse circ u lation drill h oles were drilled for a total adva n ce of 1,42 4 m. R e sults for this are tabled below (T a ble 1). Si g nificant int e rsections a re listed: DRRC12001 4.0 m @ 3.7 g/ t Au from 1 3 3.0m DRRC12010 2.0 m @ 11.5 g /t Au from 145.0m

Fi g ure 1. Dri l l hole plan showing s u rface drilli n g. M16/30 9

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Drake Resource
Drilling
Centenary Shale
Pegasus
Condemnation
Resource
Drilling
Drilling
Rubicon
Underground
Mine
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Figure 2. Pegasus K2 Long Projection

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Table 1 . Final results.

Hole ID East North RL Azi Dip EOH
Depth
From
(m)
To (m) DH
Width
Grade (g/t) Code True Width
(±0.2m)
Comment
Pegasus
PGCD12015 333061 6598068 344 61 ‐60 238.05 118.7 120.9 2.2 4.96 K2B 1.6 Preliminaryresults reported in Junequarter.
196.7 198.6 1.9 2.84 K2 1.4 Preliminaryresults reported in Junequarter.
PGCD12016 333028 6598047 343 61 ‐60 276.0 167.4 168.1 0.7 4.42 K2B 0.4
252.5 253.9 1.4 6.71 K2 Footwall
vein
1.0
PGCD12017 333041 6598100 344 61 ‐60 240.1 195.0 199 4.0 46.0 K2
Hangingwall
2.8 Preliminary results reported in June quarter.
213.0 221.9 8.9 10.4 K2 Footwall
vein
6.2 Preliminary results reported in June quarter.
PGCD12018 333031 6598118 344 61 ‐60 207.0 103.5 104.6 1.1 3.40 K2B 0.8
167.0 172.0 5.0 25.0 K2
Hangingwall
3.6
193.0 195.0 2.0 17.2 K2 Footwall
vein
1.4
PGCD12047 332902 6597980 343 62 ‐61 521.0 318.0 319.0 1.0 1.91 K2B 0.6
482.0 491.0 9.0 5.77 K2 6.2
PGCD12048 332879 6598049 343 61 ‐65 528 290.0 291.0 1.0 2.62 K2B 0.6 Preliminaryresults reported in Junequarter.
463.0 468.0 1.0 3.6 K2 0.8 Preliminary results reported in June quarter.
Screen fire results significantly downgraded
the original result
492.0 493.0 1.0 2.42 K2_CFW 0.6
PGRC12054 332958 6598276 344 61 ‐60 204 35.0 39.0 4.0 1.41 Supergene 2.8
120.0 121.0 1.0 3.28 K2_CHW 0.8
163.0 164.0 1.0 7.14 K2_CFW 0.8
PGRC12055 332923 6598261 344 61 ‐60 276 110.0 111.0 1.0 9.98 K2B 0.8
243.0 248.0 5.0 1.98 K2 3.6
PGDD12059 332884 6598154 344 61 ‐55 360.2 131.8 150.9 19.1 8.13 K2B 14.6
319.0 321.2 2.2 11.6 K2 1.6
PGDD12060 332884 6598153 344 61 ‐62 383.1 137.8 151.4 13.6 16.4 K2B 9.4
365.0 369.4 4.4 13.2 K2 3.0
PGDD12061 332792 6598115 344 ‐60 61 543.0 228.0 234.0 6.0 1.94 K2A 4.2
306.0 310.0 4.0 3.38 K2B 2.8
450.0 451.0 1.0 1.69 K2_CHW 0.8
470.0 471.0 2.0 7.55 K2_CFW 1.6
PGDD12062 332716 6598233 344 61 ‐60 549 471.0 473.6 2.6 1.84 K2B 1.8
485.0 491.4 6.4 5.62 K2 4.4
PGRC12064 332958 6598193 344 61 ‐62 270.0 94.0 132.0 38.0 7.23 K2B 26.0
229.0 230.0 1.0 1.69 K2_CFW 2.0
PGRC12065 333095 6598129 344 61 ‐61 160.0 57.0 58.0 1.0 0.34 K2B 0.6
126.0 127.0 1.0 1.34 K2_CFW 0.6
143.0 144.0 1.0 6.49 0.6 Isolated footwall intercept
PGDD12095 333061 6598086 345 61 ‐55 210.0 97.1 98.0 0.9 32.3 K2B 0.6
Hole ID East North RL Azi Dip EOH
Depth
From
(m)
To (m) DH
Width
Grade (g/t) Code True Width
(±0.2m)
Comment
172.0 172.3 0.3 2.11 K2_CFW 0.2
PGDD12096 333021 6598159 345 61 ‐55 251.5 56.0 58.5 2.5 3.42 K2B 2.0
164.0 168.0 4.0 12.7 K2_CFW 3.0
PGDD12097 333002 6598193 345 61 ‐55 216.0 52.0 53.2 1.2 1.75 K2B 1.2
118.7 119.3 0.6 21.2 0.4 Heavily fractured zone with intense
arsenopyrite alteration ‐ not a continuous
surface
146.4 150.3 4.0 1.35 K2_CHW 3.0
163.0 164.7 1.7 6.49 K2_CFW 1.2
PGRC12100 332978 6598109 343 61 ‐65 312.0 167.0 168.0 1.0 4.98 K2B 0.6
274.0 276.0 2.0 12.7 K2_CFW 1.2
PGRC12101 333046 6598070 345 61 ‐60 252.0 131.0 132.0 1.0 1.29 K2B 0.8
220.0 222.0 2.0 11.5 K2_CFW 0.8
PGRC12102 333125 6597933 343 61 ‐60 294.0 180.0 181.0 1.0 4.86 0.8 Isolated hangingwall intercept
206.0 207.0 1.0 2.18 K2_CHW 0.8 Pyrite‐rich zone with minor thin quartz veins
within victorious basalt
212.0 215.0 3.0 3.86 K2 2.2 No shale at basalt contact
PGRC12103 333038 6598311 345 61 ‐60 84.0 42.0 44.0 2.0 0.70 K2_CHW 1.4 K2_CHW in lower saprolite
70.0 71.0 1.0 0.01 K2_CFW 0.8
PGRC12104 332855 6598497 344 61 ‐60 150.0 137.0 139.0 2.0 0.17 K2_CFW 1.4
PGRC12105 332781 6598638 344 61 ‐60 180.0 116.0 124.0 5.0 0.87 K2_CHW 3.6 Includes 1m at 3.66g/t from 116‐117m
through to the logged K2 vein 120‐124m (4m
@0.13g/t)
142.0 143.0 1.0 0.02 K2_CFW 0.8 K2 vein not discernible in chips
PGDD12109 333213 6598233 345 225 ‐56 248.0 182.0 183.7 1.7 2.35 K2_CFW 0.6
PGDD12110 333335 6598024 345 265 ‐55 239.0 178.0 199.0 21.0 1.24 6.2 Footwall mineralisation ‐ Low angle intercept
213.0 220.0 7.0 5.84 K2_CHW 2.1 K2 hangingwall vein ‐ Low angle intercept
PGDD12116 333022 6598317 345 61 ‐60 82.5 55.0 59.2 4.2 9.44 K2 3.0
Drake
DDRC12001 332612 6598913 343 61 ‐60 180 113.0 114.0 1.0 1.21
118.0 120.0 2.0 1.25
131.0 140.0 9.0 2.38 K2 Incl. [email protected] from 133
DRRC12002 332629 6598877 343 61 ‐60 170 106.0 107.0 1.0 3.52 K2_CHW
116.0 121.0 5.0 1.01 K2
DRRC12004 332652 6598842 343 61 ‐60 180 133.0 136.0 3.0 2.4 K2
DRRC12005 332741 6598849 344 61 ‐60 66 29.0 38.0 9.0 1.75
DRRC12007 332732 6598822 344 61 ‐60 90 58.0 60.0 2.0 2.16 K2_CHW
DRRC12008 332682 6598769 344 61 ‐60 180 124.0 125.0 1.0 1.35 K2_CHW
DRRC12009 332740 6597853 344 61 ‐60 120 89.0 91.0 2.0 2.80
DRRC12010 332707 6598693 344 61 ‐60 198 145.0 147.0 2.0 11.5

K2 is the main mineralised surface and spans a carbonaceous shale unit, the Centenary Shale. Where the shale unit is thick and the position of the vein is distinct, K2 has been sub‐divided into the K2 vein on the footwall of the Centenary Shale (K2_CFW), and K2 vein on the hangingwall of the same shale (K2_CHW). K2B and K2A are sub‐parallel structures analogous to K2, but positioned in the hanging wall basalt. K2, K2A and K2B are all part of the same suite of shears that form part of the regional Zuleika Shear Zone.

Competency Statement

The information in this report relating to Exploration Results and Mineral Resources is based on information compiled by Mr Glenn Grayson who is a Member of the Australian Institute of Mining and Metallurgy and has sufficient exploration experience which is relevant to the style of mineralisation under consideration to qualify as a Competent Person as defined in the 2004 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr Grayson is a full time employee of Barrick Kanowna and consents to the inclusion in the report of the matters based on his information in the form and context in which it appears (Figures 1 and 2, and Table 1).