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Production, cash-flow and growth in Brazil Unlocking the potential of an emerging high-grade gold camp Mark Papendieck, Managing Director & Marcelo J de Carvalho, VP Brazil & GM Operations Simexmin, 15-18May 2016

Production, cash-flow and growth in Brazil · Production, cash-flow and growth in Brazil Unlocking the potential of an ... Mina de Ouro de alto teor produziu de 2004 a 2007 248K Oz@

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Page 1: Production, cash-flow and growth in Brazil · Production, cash-flow and growth in Brazil Unlocking the potential of an ... Mina de Ouro de alto teor produziu de 2004 a 2007 248K Oz@

Production, cash-flow and growth in Brazil Unlocking the potential of an emerging high-grade gold camp

Mark Papendieck, Managing Director &

Marcelo J de Carvalho, VP Brazil & GM Operations

Simexmin, 15-18May 2016

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Disclaimer, Forward-Looking Statements and Competent Person’s Statement

► No JORC Mineral Resources or Reserves have been defined at the Company's Projects and it is uncertain if future work will result in the definition of JORC Mineral Resources or Reserves. As such, the Company makes no representations about the grade of any potential mineralised rock that may be delivered to a mill for processing, nor can the Company make any forecasts about the potential production of ounces of gold. This presentation does not constitute investment advice. Neither this presentation nor the information contained in it constitutes an offer, invitation, solicitation or recommendation in relation to the purchase or sale of shares in any jurisdiction. This presentation does not take into account any person's particular investment objectives, financial resources or other relevant circumstances and the opinions and recommendations in this presentation are not intended to represent recommendations of particular investments to particular persons. To the fullest extent permitted by law, Orinoco Gold Limited does not make any representation or warranty, express or implied, as to the accuracy or completeness of any information, statements, opinions, estimates, forecasts or other representations contained in this presentation. No responsibility for any errors or omissions from this presentation arising out of negligence or otherwise is accepted. This presentation may include forward looking statements. Forward looking statements are only predictions and are subject to risks, uncertainties and assumptions which are outside the control of Orinoco Gold Limited . Actual values, results or events may be materially different to those expressed or implied in this presentation. Given these uncertainties, readers are cautioned not to place reliance on forward looking statements. Any forward looking statements in this presentation speak only at the date of issue of this presentation subject to any continuing obligations under applicable law, Orinoco Gold Limited do not undertake any obligation to update or revise any information or any of the forward looking statements in this presentation only changes in events, conditions or circumstances on which any such forward looking statement is based. The information in this presentation that relates to Exploration Results, Mineral Resources or Ore Reserves is based on information compiled by Dr Klaus Petersen who is a member of the Australasian Institute of Mining and Metallurgy and CREA. Dr Klaus Petersen is an employee of Orinoco Gold Limited and has sufficient experience, which is relevant to the style of mineralisation and type of deposits under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Dr Klaus Petersen consents to the inclusion in this presentation of the matters based on the information in the form and context in which it appears. It is common practice for a company to comment on and discuss its exploration in terms of target size and type. The information in this presentation relating to exploration targets should not be misunderstood or misconstrued as an estimate of Mineral Resources or Ore Reserves. Hence the terms Resource(s) or Reserve(s) have not been used in this context in this presentation. The potential quantity and grade of resource targets are conceptual in nature since there has been insufficient work completed to define them beyond exploration targets and that it is uncertain if further exploration will result in the determination of a Mineral Resource or Ore Reserve. There is information in this presentation relating to previous exploration results. Full results are included in ASX Releases and are available to view on the Company’s website www.orinocogold.com

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Brazil’s New High-Grade Gold Producer

Maiden production imminent

► Cornerstone asset – 70%-owned Cascavel Gold Mine, Brazil

► Final construction underway, commissioning June, first gold July

► Potential to become one of the world’s highest grade gold mines

► Simple gravity processing = low costs, strong margins

► Experienced team with extensive Brazilian experience

► Expertise in coarse, free-gold deposits

► Outstanding growth potential and exploration upside

► Potential for multiple production centres

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Corporate Snapshot

Our goal is to deliver strong returns for our shareholders and benefits for all of our key stakeholders by building a significant high-grade gold production business in central Brazil, leveraging off the growing cash-flows generated by the Cascavel gold mine.

ASX Code OGX

Shares on Issue 266.6M

Options on Issue

Share Price 18c

Market Capitalisation ~A$48M

Cash ~A$3.7m

Debt and Secured Hedging Nil (Forward gold sale 20% production for 3 years)

Board of Directors

John Hannaford Non-Executive Chairman

Mark Papendieck Managing Director

Ian Finch Non-Executive Director

Brian Thomas Non-Executive Director

Jonathon Challis Non-Executive Director

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Mark Papendieck – Managing Director

► 10 years working in Brazil, previously co-founder/MD of ASX-listed Centaurus Metals

Dr Klaus Petersen – President, Brazil

► Brazilian geologist +25 years experience, gold specialist

Dr Marcelo de Carvalho – VP Brazil Operations & Chief Geologist

► Brazilian geologist, previously head of Generative Exploration for TSX-listed Yamana Gold

Tim Spencer – Chief Financial Officer ► 20 years’ experience in precious metals finance/treasury roles with gold mining companies

and gold refineries

Jim Porter – Mining Consultant

► Ex-Manager of AngloGold’s Western Deep Levels (Witwatersrand)

Noel O’Brien – Process Consultant

► Ex-Managing Director of SNC Lavalin South Africa

The Team to Deliver

Key management with extensive Brazilian experience

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Cascavel Gold Mine Countdown to gold production

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Cascavel Gold Mine Countdown to gold production

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Mina Cascavel

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Ouro Alto Teor e Metais Base

► Cascavel (70%) – Nova mina de ouro de alto teor, produção em curso, excelente potencial de exploração near mine

► Sertão (OGX:100%) – Mina de Ouro de alto teor produziu de 2004 a 2007 248K Oz@ 29g/ton, mineralização aberta ao longo do plunge, excelente potencial de exploração near mine

► Tinteiro Target – Ag/Cu/Co/W alto teor

► Faina Goldfields Project (70%) – Potencial para milhões de onças de Au, IOCG, e metais base

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Geologia Regional

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► Similaridades no posicionamento tectônico-estratigráfico

► Entre os depósitos do Maciço de Goiás

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Anglo Gold

4M oz @ 7.76g/t

Yamana

1.4M oz @ 4.1g/t Yamana

300koz(?)oz

Troy

257,000 oz @ 24.95g/t

Orinoco

Cascavel target

Orinoco

Eliseu target

Orinoco

Tinteiro target : Depósitos de

Au, Cu, Ag, W relacionados a

rochas intrusivas tardas –

ocorrem em todas as

unidades

Old miners

?oz

Tectônico e Estratigráfico l

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Posicionamento

Tectônico e

Estratigráfico

Posicionamento Tectônico e Estratigráfico

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Geologia e Mineralizações Elementos Importantes

• Ciclos sedimentares compostos por base silissiclástica e associações vulcânicas

(conglomerados, grauvacas, quartzitos e pelitos) e topo caracterizado por

sedimentação química (Bifs, cherts e dolomitos)

• Unidades estratigráficas separadas por zonas de cisalhamento reversas e de

baixo ângulo (empurrões)

• Vários falhamentos de diferentes idades (Paleo P/ Brasililianos e Pós

Brasilianos) e regimes (dúcteis e rúpteis) cortam as unidades do GB

• Algumas dessas estruturas são profundas e condutos de rochas intrusivas

tardias que variam de alcalinas máficas a granodioríticas e alterações

hidrotermais associadas;

•Essas rochas intrusivas, indeformadas, ocorrem nas bordas e dentro da pilha de

rochas do GB

• Alteração hidrotermal intensa e disseminada: sericítica, clorítica, silicificação,

hematítica, magnetítica, qz+kf, carbonática, tourmalinização.

•Alterações associadas a brechas hematíticas, veios ou corpos stratabound

Principais elementos associados às mineralizações – sistema extenso e aberto

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Depósitos– Idades e Ciclos Distintos- Retrabalhamento e reciclagem – múltiplos eventos mineralizantes

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Mais velho (Archaean/Paleoproterozoic)

•Mineralização de Au associadas a estruturas de baixo ângulo e

veios de quartzo + carbonatos com halo de alteração estreito

composto por sericita, fuchsita e sulfetos (Py e AsPy); Ouro

Orogênico (Cascavel, Sertão)

• Mineralização de Au relacionadas a paleo-canais em

conglomerados e remobilizações tardias- Paleoplacer

Remobilizado (Eliseo, Sierra)

Mais jóvens (Paleoproterozoic? Neoproterozoic?

Cambrian?)

• Mineralizações de Au/Ag/Cu/Fe/W associadas a dolomitos

impuros hidrotermalizados. Associação: W e Cu. Carbonate

Replacement (Expressão distal de IOCG?)

• Sistema Polimetálico - Forte associação geoquímica entre Au,

Cu, Ni, Co, Ba, As, Ti, LREE, Mn, U, ± Ag); IOCG - Tinteiro e

várias outras ocorrências, associadas a toda a pilha de rochas.

Au ± As

Au+Cu+Ag+U+Fe

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Cascavel e Sertão- Au Orogênico

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► Depósitos relacionados a veios de quartzo em zonas de cisalhamento - ouro livre

Eliseo – Au paleoplacer

Tinteiro:

Polimetálico -

IOCG

Sertão:

Orogênic

o

Cascavel

:

Orogênic

o

Mineralização de Au associadas a estruturas de baixo

ângulo, (empurrões) e veios de quartzo + carbonatos com

halo de alteração estreito composto por sericita, fuchsita e

sulfetos (Py e AsPy); Ouro Orogênico (Cascavel, Sertão)

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Cascavel – 1740 - 2016

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Cascavel – Geologia e Mineralização

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18

(~last 20m w/ vertical scale exaggeration)

Mesre Winze

Cascavel Winze

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Cascavel – Controle Estrutural

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Lineação de intercessão = Orientação

dos shoots

Veio de Quartzo laminado com Sericita

Li // shoots

Sn-1

Veios

Sn

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Cascavel – Teor

Produção histórica - Mestre – teores +50g/t

Amostra de alto volume Mestre- 0.5 t @ 39.3 g/t Au

Amostra de alto volume Cuca- 2.7 tonnes at 27g/t Au

Amostra de alto volume Cascavel - 2.8t @ 24.1g/t Au

Amostra de Painel Cascavel - 15m @ 88g/t.

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Cascavel – Mina e Ore shoots

► Ore shoots orientados para WSW Segundo Li

► Confirmação da disposição dos shoots

► Devido efeito pepita, controle sendo realizado com amostragem de painéis (50 x 50 cm, contínuos)

► Amostra de batéia para resultados qualitativos imediatos

► Quassificação de teores:

Baixo Teor < 5g/ton

Médio 5 a 25 g/ton

Alto 25 a 100 g/ton

Super alto > 100 g/ton

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Potencial de Crescimento

► Imenso potencial de crescimento em raio de 3km do Cascavel – oportunidade de Brown Field

► Vários níveis venulados em falhas secundárias paralelas ao empurrão principal

► Essas falhas ocorrem por 20km ao lomgo de strike e já foram confirmadas 1,6km ao longo do mergulho

► Características geológicas semelhantes em todos os alvos

Controle Estrutural define novos alvos

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Mina Sertão

► Open pit (2003-2006) produziu 256koz @24.95g/t

► Localizada a 28km do Cascavel – Oportunidade de se tornar a segunda mina em operação em curto período

► Programa de sondagem preliminar 2015

• 0.5m @ 7.33g/t Au (STO_004: from 141.5-142.0m)

• 1.82m @ 13.55g/t Au (STO_005: from 130m)

• 0.65m @ 13.05g/t Au (STO_005: from 126.2m)

• 0.46m @ 21.40g/t Au (STO_005: from 131m)

• 0.5m @ 46.8g/t Au (STO_022: from 150.2m)

► Potencial de 950m ao longo do strike e 1.6km down-dip (aberto)

► 2m @ 18.7g/t Au (SRT001 de 541m de profundidade)

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Mina Sertão

Cross-section

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Polimetálico Tardio – Tinteiro IOCG

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Au ± As

Au+Cu+Ag+U+Fe

► Brechas hematíticas e gossans mineralizados aflorantes

► Alteração ferruginosa em larga escala (+ alterações potassica/sericitica e calcica-sodica)

► Anomalias geoquímica (Au/Cu) e geofísica (Grav + Mag) coincidentes com cruzamentos de estruturas regionais

► Trends marmarcados perla associação Au + Cu + Fe + Ba + Co + V + U (ppm – não ppb)

► Sondagem ao longo das falhas, afastado do centro de alteração mostram altos teores de Au (+Cu)

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Polimetálico Tardio – Tinteiro IOCG

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Tinteiro – Intrusivas e Alterações

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Sistema Tinteiro –Alteração e Introdução de Metais

17,6m@1263 ppm

Ag

2m@0,91 % Cu

4m@1137 ppm W

0,73m@ 4,8 ppm

Au

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Modelo mostra a camada de mármore, as

falhas regionais como condutos de fluidos e

possível fonte magmática, atestada pela

associação de elementos.

Sistema Tinteiro (Tardio) – Modelo

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Sistema Tinteiro (Tardio) – Modelo Regional

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Obrigado!

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Contact Information: [email protected]

Brazil’s New Gold Producer