Norilsk

  • Kavango Resources – On the road to another Norilsk in Botswana? (KAV)

    The Norilsk nickel mine sits high in the Russian Arctic plains, 1,700 miles northeast of Moscow in the permafrost of the Taimyr Peninsular.

    Here, in the Arctic Circle’s second-largest city, virtually all of Russia’s copper and Platinum Group Metals (“PGMs”) are produced. Not only that, but this polar mine accounts for 50% of the world’s palladium, some 20% of its nickel, 20% of all platinum, over 10% of the world’s cobalt, and 3% of all copper mined globally.

    This staggering production rate won’t slow down any time soon. Recent reserve estimates suggest Norilsk’s current output rates can be maintained for upwards of another 50 years. This is thanks to 500 million tonnes of probable PGM ore reserves, including 6 million tonnes of nickel, 9 million tonnes of copper, 62 million ounces of palladium, and 16 million ounces of platinum. 

    For an idea of just how valuable this mine is, consider that Norilsk’s largest shareholder is one of the richest men in Russia.

    Oligarch Vladimir Potanin swooped in for a 34.5% stake in MMC Norilsk Nickel Ltd (Nornickel) when it was privatised by the Russian government in 1995. His net worth is now reported to be close to $24 billion.

    That’s a lot of money, but it’s not just Potanin basking in Norilsk’s riches. According to the Financial Times, Norilsk has generated the highest shareholder return of any large diversified miner over the last five years. As of 2020, the company has a market value of over $40 billion - nearly twice that of Anglo American (LSE:AAL), and $10 billion more than Glencore (LSE:GLEN).

    How exciting, then, that Kavango Resources plc (LSE:KAV) is exploring a project that could rival the best of what Norilsk has to offer.

    Kavango chief executive Michael Foster has repeatedly described the company’s targets here as “highly attractive”. However, those in the know would say that this is quite the understatement.

    Kavango holds 12 prospecting licences across the KSZ and the adjacent Ditau Project in a huge, near-7,000km2 area.  Prof. David Holwell of the University of Leicester, a world authority on magmatic sulphide deposits, describes the KSZ as “a prime setting for a magmatic Ni-Cu-PGE deposit.”

    Kavango is hard at work targeting nickel-copper-platinum-group-element deposits across the 450km length of the KSZ.

    Fig. 1. Kavango’s 3 areas of exploration

    Foster is keen to draw the Norilsk comparison for one precise reason: it’s backed by geoscience.

    The same black, granular intrusive rock that hosts Siberia’s vast metal deposits – known as gabbro - is found under the Botswana sands, exactly where Kavango is drilling.

    “We believe the results from our 2019 drilling in the KSZ have brought us closer to confirming a Norilsk-style ‘plumbing system’ through which significant quantities of metal sulphides were transported,” Foster explains.

    Copper-Nickel-PGM deposits can accumulate in vast underground ‘traps’ — as molten metal-sulphides filter down through the cooling silicate magma. As at Norilsk, these accumulations can form huge ore bodies over a prolonged period of magma flow, which appears to be the case on the KSZ.

    One of the most important results from the drilling and rock sampling by Kavango to date has been the confirmation that most of the gabbroic magma intruded into sulphur-rich coal shales.

    Why is this key?

    It tells Kavango’s geologists that the sulphur content of the magma would have increased due to the incorporation of sulphur rich coal shales into the melt. Therefore, more of the valuable metals (Nickel & Copper) would have combined with the sulphur to form sulphide accumulations.

    Magmatic sulphide specialist Dr Martin Prendergast examined the geochemistry of the gabbro samples and concluded that the silicates seem to have “lost” metals during the crystallisation of the magma whilst the ratios of Cu/Zn and Cu/Pd strongly suggest that “sulphide saturation” would have occurred leading to the formation of metal sulphides. The location of these sulphide deposits are relatively simple to confirm in geophysical surveys because they conduct electricity so easily.

    In Kavango’s recent Mineral Systems Review by Prof. Holwell it is suggested that large volumes of metal sulphides including copper, nickel and platinum could be found in trap zones associated with gabbro dykes (vertical) and sills (horizontal).

    If this is correct and the accumulations are close enough to surface to mine economically, it will then be a case of identifying the location of these deposits with ground based geophysical surveys and obtaining samples of the mineralisation.

    With so much ground to cover this is obviously a big job for Kavango, but the potential rewards are huge.

    If the company is successful and identifies commercial metal deposits then this will be transformational for the company’s stock price. This will be the main focus of Kavango’s exploration efforts well into 2021.

    Fig.2. Diagram showing how metal sulphides can accumulate within sills and dykes as the gabbroic magma ascends towards the surface. (After Barnes et al 2015)

    Wider Exploration Potential in Botswana

    It’s no surprise that fellow junior mining exploration companies are now following Kavango into Botswana.

    Notably, shares in Power Metal Resources (LSE:POW) rocketed 50% in a day in April when the London explorer announced the acquisition of a 51% stake in Kavango’s Ditau Project located 70km east of the KSZ.

    At Ditau, Kavango has been focussing on 10 or so “ring structures” identified from airborne magnetic surveys, which the company believes should contain “carbonatite” lying beneath about 70m of Kalahari Sands

    Carbonatites, are intrusive/extrusive volcanic bodies whose geochemistry is dominated by calcium or magnesium carbonate. Significantly, carbonatites represent the leading source (almost the only source) of rare earth elements (REEs). REEs are becoming increasingly important in high tech applications, particularly in the manufacture of batteries and lightweight magnets used in the motors of Electric Vehicles.

    At the time of the acquisition by Power Metals, chief executive Paul Johnson said the purchase offered “a great deal of promise for highly prospective” targets of carbonatite magmatism.

    Across these targets, the Kavango/Power Metal Joint Venture hopes to discover economic deposits of REEs as well as niobium – a ductile metal used to create heat-resistant superalloys for jet engines. 

    Just 25km to the north of the project area, three carbonatites were discovered by Falconbridge Exploration in the 1970s.

    One of these was reported to contain high grades of Niobium.

    Once the Covid-19 lockdown is over, the JV partners plan to carry out orientation surveys on the Falconbridge carbonatites before undertaking an exploration exercise to identify carbonatite within the ring structures. Once carbonatites have been confirmed, shallow drilling will be employed to test for REEs and other economically viable minerals.

     

    Rising demand paints a positive picture for Copper, Nickel, REE and PGM producers

    As Kavangopushes forwards, demand for rare earths and PGMs is also soaring. More and more of the world’s technologies are coming to rely on these highly sought-after minerals

    Increasing quantities of palladium are being sought by world’s carmakers, who use the rare metal to manufacture green catalytic converters. Meanwhile, rare earths are critical in everything from medical equipment and electric car motors to lithium-ion batteries, computer hard drives, solar panels, and wind turbines.

    The net result has been a surge in prices over recent months. Palladium soared to record highs above $2,795 an ounce in January 2020.  Spot prices have remained at 25-year highs in spite of the Covid-19 pandemic.

    The reason?

    Auto manufacturers are struggling to find new suppliers and tough new emissions standards have come into force around the globe.

    Nickel, meanwhile, has jumped 18% since March.  A large driver here has been an export ban on the commodity in Indonesia – one of the world’s leading suppliers.

    So, while prices of key metals take off across the globe, and Kavango finds precisely the same underground structures that made billionaires of Norilsk investors, the company now has a huge opportunity to match this exploration potential and enrich its early investors.

    Author: Mark Sheridan

    The Author does not hold any position in the stock(s) and/or financial instrument(s) mentioned in the piece.

    MiningMaven Ltd, the owner of MiningMaven.com, owns a position in the stock(s) and/or financial instrument(s) mentioned in the piece.

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  • Kavango's hunt for elephant-scale deposits intensifies as modelling confirms Norilsk potential in Botswana (KAV)

    Kavango Resources (LSE:KAV) was trading at 2020 highs on Tuesday after confirming "spectacular" geological similarities between its vast land package in Botswana and the giant Norilsk mining centre in Russia.

    Over the past few months, Kavangohas been building a 3D model for the 450km-long Kalahari Suture Zone ("KSZ") magnetic anomaly, where it is targeting world-class mineral deposits. The area is entirely covered by Cretaceous and post-Cretaceous Kalahari sediments and has never been explored using modern techniques.

    Kavango secured thousands of data points from its own extensive aerial surveying and 2019 drill campaign, as well as from third-party historical exploration drilling and water boreholes, to build a comprehensive picture of the region’s prospectivity. On Tuesday, the company rocketed to 2.7p a share after confirming its 3D model had established critical similarities between the KSZ's northern "Hukuntsi" section and Norilsk.

    Based in Siberia, Norilsk is one of the world's biggest mining centres, accounting for 90% of Russia's nickel reserves, 55% of its copper, and virtually all of its platinum group metals ("PGMs").

    Specifically, Kavango's model depicts ten district-scale horizontal "sills" at Hukunsti covering over 300km2. Sills are relatively thin, planar, bodies of coarse-grained rock known as "solidified gabbroic magma" that intruded into layers of sedimentary rock while still molten during volcanic activity about 150 million years ago.

    According to Kavango, these sills display dozens of "gull wing" and "keel" formations that are characteristic of those containing metal-rich massive sulphides at Norilsk. Two examples can be seen in the images below.

    Cross section A-B from Hukunsti, KSZ

    Cross section C-D from Hukunsti, KSZ

    The similarities between these formations and the Norilsk schematic below are extremely striking.

    As can be seen in the Norilsk schematic below, the copper, nickel, and PGM content in the upper "gull wings" is low. Much of this metal combines with free sulphur and gravitates down as a heavy sulphide liquid into the lower "keel" sector of the sill – which can then act as a trap zone or “bowl” for massive sulphide accumulations.