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C AU T I O N A RY N OT E S A N D Q P
Certain statements in this presentation constitute forward-looking statements and as such are based on anassumed set of economic conditions and courses of action. These include estimates of future production levels,expectations regarding mine production costs, expected trends in mineral prices and statements that describeAtico Mining Corporation’s future plans, objectives or goals. There is a significant risk that actual results will vary,perhaps materially, from results projected depending on such factors as changes in general economic conditionsand financial markets, changes in prices for silver and other metals, technological and operational hazards inAtico’s mining and mine development activities, risks inherent in mineral exploration, uncertainties inherent in theestimation of mineral reserves, mineral resources, and metal recoveries, the timing and availability of financing,governmental and other approvals, political unrest or instability in countries where Atico is active, labour relationsand other risk factors.
The Company has not based its production decisions and ongoing mine production on mineral reserve estimates,preliminary economic assessments or feasibility studies, and historically such projects have increased uncertaintyand risk of failure. Mineral resources that are not mineral reserves do not have demonstrated economic viability.
Dr. Demetrius Pohl, PhD, is the Qualified Person for Atico, as defined by National Instrument 43-101. Dr. Pohl wasalso responsible for ensuring that the information contained in this presentation is an accurate summary of theoriginal reports provided to Atico and has approved the scientific and technical content of this presentation.
NON-GAAP FINANCIAL MEASURES
Cash cost per pound of payable copper produced and cash cost per tonne of processed ore are key performancemeasures that management uses to monitor performance. In addition, cash costs are an industry standard methodof comparing certain costs on a per unit basis; however, these do not have a standardized meaning and may differfrom methods used by other companies with similar descriptions. Management believes that certain investors usethese non-GAAP financial measures to evaluate the Company’s performance. These performance measures haveno meaning under IFRS and, therefore, amounts presented may not be comparable to similar data presented byother mining companies.
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G R OW T H S T R AT EGY Focused on medium-sized high grade Cu-Au assets in Latin America
Evaluate medium-sized advanced exploration opportunities in Colombia (VMS and central Cu-Au trend), Peru (southern copper belt) and Chile (northern copper belt)
Acquire mid-size private or public small scale producing mines with exploration potential
Focus on sustainable organic growth at current operation
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Principal Orogens – VMS deposits
By: 2005, Franklin et al.
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El Roble Mine’s VMS deposit is the onlyCu – Au producer in Colombia
El Roble Mine is Located in the westerncordillera of Colombia in theDepartment of Choco, near the town ofCarmen de Atrato
• >40M oz Au discovered in Colombia inthe last 10 years; discoveries in the midCauca belt Include: La Colosa (12.4M ozAu, porphyry) and Marmato (7.5 M ozAu, epithermal)
• Limited exploration activities over thepast 10 years on El Roble VMS trend
• Untested Cu-Au rich VMS large system
Major gold – copper deposits
Mining Projects in Colombia
AcandiCu-Au
PorphyrryAnglo American
MurindoCu-Au PorphyryRTZ-Muriel Co.
Buritica2.5 M Oz Au
Continental Gold
QuinchiaAu-Cu Bx Pipe
Seafield Resources Ltda.
La Colosa12.4 M oz
AuAnglogoldDominical
Au-Cu PorphyryContinental Gold
Mocoa306 M/t Cu
B2Gold
Angostura2.4 M oz Au 13.4 M oz Ag
EcoOro
Marmato7.5 M oz Au
Gran Colombia Gold
Gramalote2.4 M oz Au
B2Gold – Anglogold
El Roble MineVMS with 1.1 MT
4.9% Cu & 3.7g/t Au
Up Date to 2012
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Ore consists of copper – gold rich VMS lenses that follow the stratigraphiccontact between a thick series of Cretaceous basalt flows and overlyingsedimentary rocks.
The VMS mineralization at El Roble is hosted in a package of siliceous,carbonaceous and pyritic shales, black cherts, and minor dolomitic,graded, micritic limestones, that is up to 100m thick but averages 30m,and is known locally ‘black chert’.
The ‘black chert’ overlies a thick sequence of tholeiitic basalts withhyaclastite, and volcanic breccias. Above the ’black chert’ is a sequencelocally known as the ‘grey chert’, consisting of thin-bedded siliceous,felsic tuff interbedded with pelagic sediments. This unit varies from 30-100m thick.
The contact of the ‘black chert’ with the underlying mafic volcanics can betraced across the El Roble Project area for 10km. This lithologic packageis considered to be part of the Late Cretaceous Barroso Formation whichis in tectonic contact with a thick sequence of juvenile sandstones,mudstones and minor conglomerates of the Penderisco Formation. Bothformations are part of the Cañasgordas Group which can be traced forover 800 kilometres along the western cordillera of Colombia.
Andesite and latite dikes up to 10m thick, with an age of 18 m.y. (U-Pb,Ar/Ar) intrude both the massive sulfides and the host rocks. Sparsechalcopyrite and pyrrhotite in the dikes may be the result ofremobilization of VMS mineralization.
Age and metallogenic setting of mineralization at El Roble trend is not wellconstraine.
> 100Km underexplored VMS trend
Regional geology
Underexplored VMS Cu – Au Trend
El Roble MineVMS
Alacran - VMS
Anza- VMS
El Dovio- VMS
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VMS deposits typically occur in clusters
VMS Geological Model
• VMS deposit • VMS deposits typically occur in clusters
• Schematic of a massive sulphide deposit zonation typical of chalcopyrite - pyrite ± pyrrhotitein the lower part
• Volcanogenic massive sulphide (VMS) deposits are a well-defined deposit type.
• Franklin et al. (2005) cite 804 known examples around theworld. By 2009, the number had grown to 1090 (Mosier et al.,2009).
• VMS deposits are defined by Franklin et al. (2005) as“stratabound accumulations of sulphide minerals thatprecipitated at or near the sea floor in spatial, temporal andgenetic association with contemporaneous volcanism.”
• Given the large number of mafic-type VMS deposits around theworld, one can predict the size and grade of future discoveriesbased on the grade and tonnage distribution of knowndeposits.
• VMS deposits, including mafic-type VMS deposits, typicallyoccur in clusters. A cluster of mafic-type VMS deposits can, inaggregate, be considerably larger. The aggregate size depends,logically, on the number and characteristics of the individualVMS deposits that make up the cluster.
• The largest VMS deposits in South America are the TamboGrande deposits (Winter et al., 2010) of northern Peru(including Tambo Grande One: 109 Mt of 1.6% Cu, 1.0% Zn, 0.5g/t Au, 22 g/t Ag; Tambo Grande Two: 82 Mt of 1.0 % Cu, 1.4 %Zn, and 0.8 g/t Au, 25 g/t Ag; Tambo Grande Three; and B5).There are also several clusters of VMS deposits in the westernCordillera of central Peru (Moro, Cerro Blanco, Maria Teresa,Aurora Augusta, Santa Cruz de Cocachara, Palma, Balducho,and Cerro Lindo deposits).
Massive sulphide
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Location map
El Roble Cu - Au Mine, Colombia
El Roble mine is the only Cu-Au VMS deposit in production in Colombia
3.5 hours away from the city of Medellin via paved 145 kilometer highway
Power grid, abundant water and mine facilities on site
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R EG I O N A L G EO LO GY
Stratigraphic Column
Regional Geological Map
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S t r u c t u ra l S e t t i n gI d e a l M o d e l
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Ideal Model in Andean Coordillera
All of the above rock units were affected by folding, faulting andthrust tectonics during Late Cretaceous to Tertiary accretion tocontinental South America. Accretionary tectonics resulted inboth low-angle and high-angle faulting of the stratigraphy anddismembered the deposit into discrete ore lenses. At the ElRoble mine the VMS host lithology appears to be overturned,dips steeply to the east and appears to be in thrust contact withthe structurally underlying sediments of the PenderiscoFormation
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E L R O B L E M I N E D I S T R I C T E X P L O R AT I O N U P S I D E
Atico identified and mapped a 10 km stratigraphic contact between basalt flows and pelagic sediments that control mineralization
Geochemical program(1) and geophysical surveys(2) have outlined multiple VMS targets over the 10 km favorable contact
Only 2 of 15 district geochemical targets have been previously drilled; Archie and Santa Anita
Atico plans to drill at least 2 targets in 2016
Potential for more targets to be discovered during district exploration of the heavily vegetated terrain
Potential to discover additional VMS bodies
(1) Geochemical program corresponds to rock chip and soil sampling(2) Geophysical surveys conducted include IP, VTEM, magnetic survey,
gravity and down-hole EM Geological map of favorable contact within El Roble claims
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B r o nw f i e l d E x p l o ra t i o n – C o n c e p t u a l M o d e l
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B r o nw f i e l d E x p l o ra t i o n – C o n c e p t u a l M o d e l
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B r o nw f i e l d E x p l o ra t i o n – S a nta A n i ta
Ag KNa
DDHAlto Mod. Bajo
SuelosAlto Mod. Bajo
RocasDDH - MINER
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B r o nw f i e l d E x p l o ra t i o n– Pa t h f i n d e r E l e m e nt s
Ba Na AlK
San Lorenzo
Santa Anita
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B r o nw f i e l d E x p l o ra t i o n– C C P I v e c to r
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Geophysics Target
Ground Magnetic Targets Ground Magnetic Targets – Geology
Carmen de Atrato
El Roble Mine
M a g n e t i c S u r ve y Re s u l t s
All geochemical anomalies confirmed
Most magnetic anomalies align well along the 10 kilometer favorable contact
42 new Gmag targets detected which have not been considered in past exploration programs
Carmen de Atrato
El Roble Mine
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B B’
B B’
Gmag & Geoq. Au
E x p l o ra c i ó n B r o nw f i e l d – S a n L o r e n zo
• Geología Favorable (Black Chert )• Geoquímica Au, Ag, Zn ‘ Anomalía Metales Base.• Gmag – Favorable.• VTEM – Resistividad.
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E L R O B L E M I N E V I C I N I T Y E X P L O R AT I O N P R O G R A M
High grade mineralization continues at depth
Intercept (m)
Body Hole ID From To Interval (m) Cu (%) Au (g/t) Ag (g/t)
Goliath ATDHR-01 109.2 151.0 41.7 6.54 1.82 7.43
Including 109.2 111.0 1.7 9.00 4.81 22.2
121.0 123.0 2.0 6.87 10.27 11.4
125.0 141.0 16.0 7.13 1.00 3.87
143.0 145.0 2.0 14.85 0.91 15.15
ATDHR-12 113.9 132.1 18.15 10.30 2.10 6.59
Including 113.9 118.0 4.10 11.06 6.46 17.57
120.0 122.0 2.00 15.91 0.78 3.23
122.0 126.0 4.00 17.45 1.06 3.94
ATDHR-20 128.0 148.4 20.40 5.25 1.28 6.16
Maximus ATDHR-04 61.0 102.0 41.0 6.49 17.57 13.26
Including 75.0 85.0 10.0 3.00 3.59 12.77
85.0 95.0 10.0 18.40 8.63 19.29
95.0 97.0 2.0 3.92 250.0 21.2
97.0 102.0 5.0 6.05 7.21 13.20
ATDHR-05 70.0 79.0 9.0 2.50 2.31 16.17
Including 75.5 77.0 1.5 3.81 9.41 145.5
77.0 78.0 1.0 10.82 1.60 0.00
ATDHR-17 71.8 160.5 88.70 5.41 2.48 10.83
Including 71.8 75.2 3.40 11.50 7.22 13.77
100.3 104.1 3.80 7.17 3.89 18.20
141.1 149.5 8.45 12.96 1.09 12.70
Zeus ATDHR-26 144.0 263.7 119.7 6.89 6.26 16.50
Including 145.8 156.3 10.43 11.68 14.14 33.83
ATD-0003 158.8 245.20 86.4 5.04 3.71 8.69
ATD-0004 155.7 225.75 70.1 6.26 1.85 7.93
Including 186.4 225.75 39.53 7.50 1.31 5.67
ATDHR-28 242.8 292.0 49.20 4.11 2.32 6.36
Including 257.4 266.5 9.12 6.69 1.71 7.07
2012-15 Exploration Highlights
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E l Ro b l e M i n eMine overview
Administrativeoffices
Mill
Core shack
Tailings dam in remediation
El Roble Mine, Colombia
New 1880 adit
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The historic mine operated since 1990’s. An operation with a room and pillar method and concluded recovering the remaining ore through sublevel caving.
Operated with jackleg for drilling, scoop for ore load and mine wagon for ore haulage.
H I S TO R I C M I N ELV L . 2 0 0 0 a n d 2 1 0 0
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E L R O B L E M I N E , C O LO M B I AMajor scale-up components completed to achieve 800tpd
New tailings facilityEntrance to new level 1880 adit
First and second phase of the new tailings facility completed
Facility built to international standards
Third phase construction will commence as required by operational needs
Five by five, 830 meter adit
Direct access to the newly discovered resources
Improved underground drill access
Capacity beyond 800tpd
800 tpd processing facility
Upgrades to the crushing and milling circuit including a new cone crusher and stronger ball mill motors
Additional flotation cells
Upgrades to the thickener and vacuum drum filter
New on site lab
ADIT TAILINGS FACILITY PROCESSING FACILITY
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E L R O B L E M I N E , C O LO M B I A In production for over 22 years
Location Carmen de Atrato, Colombia
Ownership 90%
Type of deposit Mafic-type Volcanic Massive Sulphide
Commodities Cu, Au, Ag
Processing Standard grinding, milling and flotation circuit
Operation 800 tpd underground mine
End Product Cu (+Au,Ag) Concentrate
M&I Resource 1.87Mt at 3.46% Copper, 2.27g/t Gold
800 tpd processing facility
*
*
* During the option term and up to November 22nd 2013, the Company was not responsible for mining or for resource development and gained no income from the mining operations
** The Company is basing 2017 guidance on year ended December 31, 2016 financial and production results. Please refer to Cautionary Note on Forward Looking Statements at the beginning of this document.
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**
**
1,412
9,07912,044
18,724
543%
33%
55%
0
2,000
4,000
6,000
8,000
10,000
12,000
14,000
16,000
18,000
20,000
2013 2014 2015 2016 2017
(00
0s)
lbs
Copper Production
2,297
9,53810,994 11,159315%
15%
2%
0
2,000
4,000
6,000
8,000
10,000
12,000
2013 2014 2015 2016 2017
oz
Gold Production
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E L R O B L E E X P L O R AT I O N U P S I D E
El Roble Mine Area and Archie Target
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E L R O B L E M I N E D I S T R I C T E X P L O R AT I O N U P S I D E
Atico identified and mapped a 10 km stratigraphic contact between basalt flows and pelagic sediments that control mineralization
Geochemical program(1) and geophysical surveys(2) have outlined multiple VMS targets over the 10 km favorable contact
Only 2 of 15 district geochemical targets have been previously drilled; Archie and Santa Anita
Atico plans to drill at least 2 targets in 2016
Potential for more targets to be discovered during district exploration of the heavily vegetated terrain
Potential to discover additional VMS bodies
(1) Geochemical program corresponds to rock chip and soil sampling(2) Geophysical surveys conducted include IP, VTEM, magnetic survey,
gravity and down-hole EM Geological map of favorable contact within El Roble claims
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CORPORATE OFFICESuite 501 – 543 Granville St.Vancouver BC V6C 1X8T: +1.604.633.9022
C O N TA C T I N F O R M AT I O N
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CORPORATE DEVELOPMENTIgor [email protected]
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