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Appendix A
 
 

ORE RESERVES AND MINERAL RESOURCES REVIEW

 
CONVERTING RESOURCES TO RESERVES
 
Total Proved Ore Reserves increased from 809 million tonnes in 2007 to 854 million tonnes in 2008 primarily due to higher confidence in the ore bodies at Rustenburg and Amandelbult mines’ UG2 deposits. Outside of South Africa’s Bushveld Complex, Anglo Platinum continued to explore in Brazil, Canada, China, Russia and Zimbabwe in 2008.

In line with Anglo Platinum’s review and audit schedule, the external Mineral Resource and Ore Reserve process review will next be conducted during 2009.
Bridgid Moyo is a transport assistant who works underground at Union Mine. Transport assistants direct the movement of locomotives.
 

THE BUSHVELD COMPLEX

The resources of platinum group metals (PGMs) that result in Anglo Platinum’s major competitive edge reside mostly in South Africa’s uniquely large, mineral-endowed, layered igneous intrusion known as the Bushveld Complex. This complex remains the world’s largest source of platinum, despite substantial exploration effort and funding in other parts of the world to find a body of rock that can match it.

Formed just over 2,000 million years ago, when molten rock known as magma was injected into the upper reaches of the earth’s crust from chambers deep below, the Bushveld Complex is an enormous, irregularly shaped saucer 350 kilometres across, with its central area deep underground but it’s commercially valuable rim exposed at or near the surface on its western, eastern and northern sides, or ‘limbs’. At the outer edges of each of the limbs, rocks known as pyroxenites, norites, gabbros and chromitites are found interlayered in a variety of combinations that make up several readily identifiable zones extending the length and breadth of the complex. Within these zones are a number of orebodies that yield a variety of minerals, including chromite, titaniferous magnetite, vanadium pentoxide, nickel, copper and, more importantly for Anglo Platinum, the PGMs.

Within the sequences of rocks, there are three distinct layers that contain concentrations of PGMs at levels that are currently economic to mine. Other layers in the Bushveld Complex sequences also carry PGMs, but none of them can currently be extracted on the basis of PGM content alone. (Even where PGMs have been produced as by-products, the quantities have been insignificant in world terms.)

The principal PGM-bearing horizons being exploited remain the Merensky Reef and the Upper Group 2 (UG2) Reef, which occur around the Eastern and Western Limbs of the complex, while a third PGM-rich layer, the Platreef, is found only on the Northern Limb, at the northeastern north-eastern edge. In 2007, it was reported that there are other deposits geologically similar to Platreef in some respects, such as the Sheba’s Ridge deposit as yet these have not, however, been able to support the development of a mining project and therefore are yet to be mined.

The Merensky Reef has been the principal source of PGMs since it was first worked in 1925. However, the other reefs have grown steadily in importance. By 1999, the Merensky Reef accounted for only 50% of all platinum-bearing ore processed in South Africa. Exploitation of the UG2 Reef began in the 1970s and has steadily increased; in 1999, it was the source of 42% of ore processed. This is now thought to have increased to more than 50% across the complex. The UG2 is found at a vertical distance of between 16 and 400 metres below the Merensky Reef, depending on location. The Platreef, mined briefly in the 1920s, was first exploited on a large scale in 1993 and is gradually becoming a significant contributor of PGMs for Anglo Platinum.

Although narrow – the Merensky and UG2 reefs are generally mined at a stoping width of less than a metre – these tabular orebodies extend laterally over hundreds of square kilometres, resulting in extensive Mineral Resources, the continuity of which, established over years of exploration and mining, permits the long-range extrapolation of data.

On the Northern Limb of the Bushveld, the UG2 Reef is not developed on Anglo Platinum’s properties. On the other hand, the Platreef, which is substantially thicker than either the Merensky Reef or the UG2, is well developed on these properties. The term ‘Platreef’ describes zones of mineralisation occurring in a variety of rocks that range from normal pyroxenites to a host of rock types that have arisen through the contamination of Bushveld magma by sediments from the underlying Transvaal Supergroup. The thicknesses of Platreef are such that they can support open-pit mining operations to depths well in excess of 200 metres at current prices and mining costs. Significantly, they provide a much safer mining environment than does underground mining.

The Merensky Reef and the Platreef yield meaningful quantities of nickel and copper as by-products of PGMs. The UG2 is relatively devoid of nickel and copper, and although chromitite in this reef has potential for economic gain and in some areas is being exploited in this way, we have not considered this when measuring the contained monetary values for Ore Reserve purposes. However, other non-significant UG2 base metals have been considered, and their value has been accounted for in the relevant economic evaluations. 
 

OVERVIEW OF EXPLORATION 

Exploration 2008

The exploration department operated well within the safety standards that were set at the beginning of the year, and no significant negative incidences were recorded.

Extensive exploration activities on all Anglo Platinum properties continued once again, with a total of 470,050 metres of diamond drilling completed in 2008. This very significant effort is in line with the requirements for Resources set by the Company’s project portfolio for new developments and mine planning, and the conversion of Resources to Reserves where the latter occurs in proximity to operations. Prospecting based on recently issued prospecting permits is progressing in line with the works programme schedules.

As was the case in 2007, the main focus of exploration work in 2008 was risk mitigation and the upgrading of resources where appropriate. Anglo Platinum has an impressive portfolio of announced and upcoming projects. These are being assessed in line with internationally recognised best practice, as attested to by both in-house and international third-party reviewers. Drilling remains a primary tool in determining and evaluating resources, and the extensive and structured drilling programmes reflect this systematic approach to generating value for the organisation. Although some percussion drilling is used for specific needs, diamond drilling, using mostly BQ (48 mm) diameter coring, is used for some 99% of boreholes drilled. Only reef intersections with 100% core recovery are used in the geological models of resource grades.

Advances in the technology of three-dimensional seismic surveys have been used fully by the exploration team in recent years. These surveys continue to be an invaluable tool for supplementing borehole data, by providing exceptional detail on the structural deformation of the orebodies, which is not discernable from borehole data alone. This ensures the correct placement of shafts and other critical mining infrastructure, particularly where orebodies are at moderate to deep depths. Several additional surveys are also in the planning stage and will be implemented, subject to cost and access considerations. Aeromagnetic surveys, geophysical logging and borehole radar are also used to supplement geological knowledge on each of the prospects.

Where mine planning has reached an advanced stage, a variety of additional drillhole and surface to near-surface imaging tools are employed, to determine the structure and competency of the ground targeted for development. In-drillhole and rock surface remote sensing are integral components of this risk-mitigation process: they have proved highly cost beneficial over recent years.

Foreign exploration continued in 2008, with the ongoing objective of finding, locating and defining projects of value to the organisation. This included projects in Brazil, Canada, China, Russia and Zimbabwe, with watching briefs in a number of other promising geological provinces. Our goal remains to be able to evaluate projects swiftly and promote them promptly where appropriate, with an information system in place to promote these objectives.
 
Seismic survey control room.
 
Russia: Two projects are being explored, with differing styles of mineralisation. In the Urals, an alluvial platinum target is reaching an advanced stage, with appropriate documentation shortly to be filed. If approved, this will permit exploratory mining to validate exploration results. Several other placer occurrences are under review and being tested, each with a high potential to become a resource evaluation target. These deposits are dominated by platinum mineralisation, with the metal occurring as ferroplatinum alloy in nugget form and individual nuggets comprised of around 90% platinum. Concentrations of platinum in the ore are in the order of a few grams per cubic metre.

In the Kola Peninsula, three large areas of greenfields exploration remain our focus. Where diamond drilling has been used as the main tool for exploration, it has revealed mineralised zones of considerable interest in two areas to date. Geophysical surveys are assisting in target generation and drillhole-siting programmes.

Canada: The River Valley project progressed to the level of a pre-feasibility study. This indicated that, under present economic circumstances, the deposit is not viable. The process of acquiring a lease over the property was concluded, which will facilitate its retention until market conditions permit mining, or permit a sale of the rights in future. Adjoining ground evaluation and regional targeting – the objective of our 2007 field season’s activity – were followed up on in 2008, but no additional potential was identified.

China: The extensive Panxi Rift in south-western Sizhuan Province has been the primary geological target area in China, with the local focal points of activity being a number of specific intrusive complexes. The Emeishan basalt suite of flood basalts is emplaced above conducive and reactive country rocks, creating a mineralisation environment similar to the one Anglo Platinum is familiar with in South Africa. A range of occurrences and anomalies were identified. Some were considered worthy of an application for a special prospecting licence. These applications were under consideration by the Chinese authorities during the year.

Unfortunately, drilling in the Danba project area did not provide sufficient encouragement to continue prospecting this deposit; work there has been discontinued.

Brazil: Ongoing mapping and geophysically targeted drilling progressed well during the 2008 field season, with target identification strategies being successfully applied. The work remains focused on a geological terrain conducive to the development of chromite- and sulphide-associated PGEs within igneous intrusives.

Zimbabwe: Resource definition and quantification within and outside the Unki resource block were completed during 2008. Prospective resources additional to the Unki resource were successfully defined. Exploration activity has been maintained, pending the finalisation of ongoing government negotiations.

In March 2008, an agreement was entered into with the Government of Zimbabwe (GOZ) in terms of which 31.3% of the PGM mining claims have been released to GOZ in return for cash and empowerment credits. The agreement is expected to become effective during 2009.

Western Bushveld Joint Venture: In 2004, Rustenburg Mine entered into a joint-venture agreement with Platinum Group Metals RSA Limited and Africa Wide Mineral Prospecting and Exploration (Proprietary) Limited, to establish the Western Bushveld Joint Venture. Wesizwe Platinum Limited acquired Africa Wide Mineral Prospecting and Exploration in September 2007. In mid-2008, the Western Bushveld Joint Venture completed a bankable feasibility study for its Project 1 area.

In December 2008, RPM entered into agreement to sell its interest in the WBJV to Wesizwe Platinum Limited. The parties are currently in the process of fulfilling the suspensive conditions of the agreement.

Sheba’s Ridge Joint Venture: Sheba’s Ridge Joint Venture is a project owned jointly between Ridge Mining (65%) and Anglo Platinum (35%). Ridge Mining agreed to sell to the Industrial Development Corporation of South Africa a 26% interest in the joint venture in return for funding of R60 million to complete a feasibility study on the project. Ridge Mining has completed the feasibility study with the exception of the process strategy.
 
Ron Hieber (Pr Sci Nat, FGSSA, MCIM)
Head: Exploration and Mineral Strategy

Johannesburg
5 February 2009
 
 
 
 
CHANGES IN THE ORE RESERVES AND MINERAL RESOURCES
STATEMENT FOR 2008

ORE RESERVE – MINERAL RESOURCE SUMMARY

  2008 2007

Category
Million
tonnes
4E million
troy ounces
Million
tonnes
4E million
troy ounces
Total Ore Reserves 1,478.3 197.5 1,453.3 194.1
Proved Ore Reserves 853.6 108.4 808.6 104.6
Total Mineral Resources 5,203.1 654.7 5,696.2 720.0
Measured Mineral Resources 607.8 92.0 621.8 91.1
Measured and Indicated Mineral Resources 2,221.1 280.6 2,188.6 280.8
The total Ore Reserves increased primarily due to the conversion of additional Mineral Resources to Ore Reserves at:
  Amandelbult Mine (Merensky Reef and UG2 Reef ); and
  Rustenburg MIne (Merensky Reef and UG2 Reef ).
  This resulted in a 1.7% tonnage increase and a 1.8% 4E ounce increase.
The Proved Ore Reserves increased primarily due to higher confidence from:
  Rustenburg Mine (UG2 Reef ) where additional drilling and re-evaluation resulted in higher confidence and due to improved modifying factors; and
  Amandelbult Mine (UG2 Reef ) where additional drilling and re-evaluation resulted in higher confidence.
  This resulted in a 5.6% tonnage increase and a 3.7% 4E ounce increase.
The total Mineral Resource tonnage (additional to the Ore Reserves) has decreased considerably, mainly due to the successful transaction announced with Mvelaphanda Resources and the consequent exclusion of the Mineral Resources of the Booysendal project. This resulted in a 8.7% tonnage decrease and a 9.1% 4E ounce decrease in total Mineral Resources.
The overall Measured and Indicated Mineral Resources changed marginally. The tonnage increases by 1.5% and the 4E ounce decreases by 0.1%.

For detailed statistics refer to Company statistics. 

GLOSSARY FOR WATERFALL GRAPHS

Opening balance: As at 31 December 2007.
Production: The quantity of the commodity of interest delivered for beneficiation from underground or open-pit including material from stockpiles (mine depletion during the financial year).
Conversion: Process of converting Mineral Resources to Ore Reserves .
Conversion (reallocation): Process of ‘down-grading’ of Ore Reserves to Mineral Resources.
Disposal: Reduced Ore Reserves/Mineral Resources due to new JV agreements (Transaction with Mvelaphanda Resources).
New information: The effect of additional resource definition information which initiates an update to the geological models (facies, structural, grade, geo-technical) and results in a new (reclassified) resource model.
Exploration: Includes ore bodies not previously reported.
4E grade: sum of platinum, palladium, rhodium and gold grades.
MR: Merensky Reef.
Closing balance: As at 31 December 2008.
 
 
 
   
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