Pjx Resources Inc. · TSXV:PJX
Pjx Resources — Investor Presentation (February 2018)
44 slides from Pjx Resources's investor presentation, February 2018
Slide 1: Base Metal Potential (Zinc, Lead, Copper)
Base Metal Potential (Zinc, Lead, Copper) February 2018 (TSX-V: PJX)
Slide 2: Disclaimer
Disclaimer Some of the information in this presentation has been extracted from the prospectus and NI 43-101 Technical Report filed on SEDAR (www.sedar.com). Investors should base their investment decision on information contained in the prospectus and NI 43-101 Technical Report only. This presentat
Slide 3: PJX Resources' Cranbrook Area Gold & Base Metal Properties
PJX RESOURCES’ CRANBROOK AREA GOLD & BASE METAL PROPERTIES 3
Slide 4: Mineral Potential of the Belt-Purcell rocks near Cranbrook
Mineral Potential of the Belt-Purcell rocks in Canada and USA near Cranbrook • Regional underlying Structural Zones appear to influence location of large deposits and mining camps. • Sullivan Mine and Kimberly Gold Trend, occur above the regional Kanasewich (Vulcan) Structural Zone. - Vine, Dewdney
Slide 5: Deposit Potential Map Canada–USA Border in Cranbrook Area
Deposit Potential Map Canada – USA Border in Cranbrook Area • Deposits (Sullivan, Coeur d’Alene, Montanore) occur along or proximal to where east-west oriented structural zones create breaks or bends in north- south structures. • Major break occurs where the east-west oriented Vulcan-Kanasewich Stru
Slide 6: Summary
Summary • PJX owns 100% mineral rights to large land package in historical mining camp. • Over $20 million in historical data has been compiled. • Data Gaps addressed by new exploration technologies and techniques. • Numerous large gold, silver, zinc-lead, and copper targets have been identified. •
Slide 7: Sedimentary Exhalative (SEDEX) Deposit Model
Sedimentary Exhalative (SEDEX) Deposit Model Massive Sulphide Ore (zinc, lead, silver) (Image: Imperial College, William-Turner) • Ocean floor is sinking along syn- sedimentary growth faults forming a fault scarp and a 3rd order basin. (Zinc, Lead, Silver) • Faults act as a pathway for fluids to des
Slide 8: Regional Geology Map
Regional Geology Map • Vine and Fors discoveries occur at intersection of growth faults similar to the Sullivan Deposit. • The Vine Graben is considered as possible southern extension of the Sullivan Graben that hosts the Sullivan Deposit. • Sullivan Deposit was a Sedex (Sedimentary Exhalative) styl
Slide 9: Vine Property (Historical Vein Structure at Surface)
Vine Property (Historical Vein Structure at Surface) 9
Slide 10: Vine Core Facility and Core Racks
Vine Core Facility and Core Racks (February, 2015) Vine Vein 10
Slide 11: Core Storage
Core Storage 11
Slide 12: Core Logging Facility
Core Logging Facility 12
Slide 13: Detailed Ground Gravity
• Detailed ground Gravity Geophysical Surveys have identified 2 Gravity Target Areas (East and West targets) on the Vine Property. • Gravity identifies changes in rock density. • Massive sulphide mineralization found at the Sullivan Deposit is very dense material that would form a gravity anomaly. •
Slide 14: Vine Property - Interpreted Geological Cross Section WW
Vine Property - Interpreted Geological Cross Section WW Sedex Massive Sulphide • Massive Sulphide with zinc, lead and silver mineralization was intersected by historical drill holes KV90-41 and KV94-57 at the base of the Footwall Quartzite (FWQ horizon). (Note: KV90-41 and KV94-57 drill hole data sh
Slide 15: Sphalerite replacing sediments along fractures
Sphalerite (zinc-sulphide) replacing sediments along fractures intersected below the gabbro sill and above the attenuated - deformed zone of the Moyie Fault. 15
Slide 16: Folded Lower Aldridge
Folded Lower Aldridge Sediments in the attenuated – deformed zone above the Moyie Fault. 16
Slide 17: Folded Lower Aldridge Sediments
Folded Lower Aldridge Sediments in the attenuated – deformed zone above the Moyie Fault. 17
Slide 18: Folded, irregular Sulphide
Folded, irregular Sulphide mineralization with zinc and copper in the attenuated – deformed zone above the Moyie Fault. 18
Slide 19: Broken Hill Deposit
Broken Hill Deposit • Sedex style Massive Sulphide folded within the deformed – attenuation zone of a major fault (shear zone). • The folded style of massive sulphide mineralization at the Broken Hill Deposit may Folded – irregular shaped occur at the Vine Massive Sulphide (Ore Lens) Property along
Slide 20: Massive Iron Sulphides
Massive Iron Sulphides (Pyrite and Pyrrhotite in folded metamorphosed zone above the Moyie fault – about 2 km west of East Gravity anomaly). Intense Albite (white mineral) and Chlorite (dark green mineral) alteration often associated with Sedex massive sulphide deposits. 20
Slide 21: Broad zone with mineralization on the East Gravity Anomaly
Broad zone with mineralization on the East Gravity Anomaly • Anomalous sphalerite (zinc) mineralization locally occurs disseminated, or as veins, or bands within a broad zone approximately 100 metres true width. The zone has been traced in drill holes for about 500 metres and is open to the north, w
Slide 22: Enlarged view of mineralized band
Enlarged view of mineralized band in previous slide Galena (grey – silver colour, lead mineral). Sphalerite (reddish brown colour, zinc mineral). 22
Slide 23: Sphalerite
Sphalerite Brown coloured zinc mineralization in phyllite rock within folded metamorphosed zone above the Moyie fault) 23
Slide 24: Sphalerite
Sphalerite Brown coloured zinc mineralization in vein cutting Gabbro about 300 m above the folded metamorphosed zone. 24
Slide 25: Sphalerite
Sphalerite Brown coloured zinc mineralization in fractures cutting Gabbro about 300 m above the folded metamorphosed zone. 25
Slide 26: Gravity Profile along Geological Cross Section UU
Gravity Profile along Geological Cross Section UU Interpretation of the Gravity data suggests that massive sulphide (shown in red) may occur above and folded within the attenuated - deformed zone above the Moyie Fault 26
Slide 27: View looking west from the West Gravity Target
View looking west from the West Gravity Target toward CPR’s Railyard and Rock Quarry CPR Quarry Highway 3 CPR Railyard 27
Slide 28: Vine Property Target Locations and Infrastructure
Vine Property Target Locations and Infrastructure • Target areas are located 12 km south of Cranbrook, British Columbia. • Property is accessible by road year round. • Highway 3, CPR Rail, and 2 Power Transmission Lines cross the Property. • CPR Rail Yard for loading rock from a CPR quarry is locate
Slide 29: Rail Lines Western Canada and Northwest USA
Rail Lines Western Canada and Northwest USA • CPR rail line crosses the Vine Property. • Teck’s Trail zinc-lead- silver smelter and metallurgical complex is approximately 145 km west of the Vine Property. • Rail also provides access across North America and to the coast with shipping to Asia or othe
Slide 30: DD Property
DD Property • Potential to Host Sullivan type Zinc-Lead-Silver Deposit. • 2015 – Teck Resources Limited stakes land adjacent to PJX’s properties along the Moyie Fault Structure. • 2016 – Teck Options DD Property from PJX Resources. • 2018 – Teck plans to drill Sullivan deposit type target identified
Slide 31: Copper Showings Dewdney Trail and Zinger Properties
Copper Showings Dewdney Trail and Zinger Properties Copper Cliff Showing • Multiple copper showings occur on both properties (red dots). • Sedex style copper mineralization occurs at the Hope Copper Copper Cliff, Hope, and other Showing showings on the both properties. • Intrusive related copper min
Slide 32: Dewdney Trail Property Copper Cliff Showing
Dewdney Trail Property Copper Cliff Showing • Chalcopyrite and Malachite (copper) mineralization in Proterozoic age sediments. • Potential for Sedex style copper deposits. • Montanore, Spar Lake, Rock Creek Sedex copper deposits occur to the south in Idaho. 32
Slide 33: Dewdney Trail Property Copper Cliff Showing
Dewdney Trail Property Copper Cliff Showing • Fracture and bedding controlled Chalcopyrite and Malachite (copper) mineralization. • Proterozoic age white quartzites. 33
Slide 34: Copper Cliff Showing
Fracture and bedding controlled chalcopyrite and malachite (copper mineralization) in quartzites. Copper Cliff Showing 34
Slide 35: Dewdney Trail Property New Copper Showing - 2017
Dewdney Trail Property New Copper Showing - 2017 Chalcocite & Malachite in quartzite New showing discovered 700 metres from Copper Cliff Showing 35
Slide 36: Zinger Property Hope Copper Showing
Zinger Property Hope Copper Showing Malachite (green copper mineral) in altered quartzites 36
Slide 37: Zinger Property Hope Copper Showing
Zinger Property Hope Copper Showing Bornite in altered quartzites 37
Slide 38: Zinger Property
Zinger Property • Copper (Chalcopyrite, Malachite) mineralization in altered middle Creston (Rivett) quartzite. • Fracture and bedding controlled mineralization. • Copper showing is a few hundred metres stratigraphically below the Hope Bornite Showing. 38
Slide 39: Summary
Summary • PJX owns 100% mineral rights to large land package in historical mining camp. • Over $20 million in historical data has been compiled. • Data Gaps addressed by new exploration technologies and techniques. • Numerous large gold, silver, zinc-lead, and copper targets have been identified. •
Slide 40: PJX Capital Structure
PJX Capital Structure Listed on TSX Venture Exchange (PJX.V) Share Structure Current as of June 2017 Shares Issued: 75,913,396 Warrants: 31,837,571 Options: 6,023,500 40
Slide 41: Directors' and Officers' Biographies
Directors’ and Officers’ Biographies • John Keating, PGeo – Chief Executive Officer, President and Director Mr. Keating has over 35 years of experience in the mining and exploration industry. He conducted early and advanced stage exploration with Noranda and was a global commodity analyst for gold,
Slide 42: Directors' and Officers' Biographies
Directors’ and Officers’ Biographies •Kent Pearson, PGeo – Director Kent Pearson is a professional geologist with more than 25 years of experience in the mining industry and in the capital markets sector. His mining experience spans from grassroots exploration through to mine production. In the capi
Slide 43: Consultants' Biographies
Consultants’ Biographies Dr. Trygve Hoy, P.Eng Dr. Hoy is a Professional Engineer with 40 years of mineral industry experience working as a research economic geologist with the British Columbia Department of Mines prior to consulting on mineral properties for the private sector. His experience and e
Slide 44: For Additional Information Contact: PJX Resources Inc.
For Additional Information Contact: PJX Resources Inc. 5600 – 100 King Street West Toronto Ontario M5X 1C9 416-799-9205 [email protected] Attention: Linda Brennan or visit our web site at: www.pjxresources.com 44
PJX Resources — Investor Presentation (February 2018) on 6ix