Disclaimer Some of the information in this presentation has been - - PowerPoint PPT Presentation

Vine Property Zinc, Lead, Silver Deposit Potential

August 2015 (TSX-V: PJX)

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 presentation may contain certain forward looking information relating to expected future events and financial and operating results of the Company that involve risks and

• uncertainties. Readers are cautioned not to place undue reliance on forward-looking

statements as there can be no assurance that the plans, intentions or expectations upon which they are based will occur. Due to the potential impact of various factors, including the volatility of metal prices, new information regarding recoverable reserves or resources, market competition, changes in environmental and other regulations, political changes, and other factors, the Company disclaims any intention or obligation to update or revise any forward-looking information, where as a result of new information, future events or otherwise, unless required by applicable law. Geological information has been reviewed by John Keating, P.Geo. (a qualified person for the purpose of National Instrument 43-101 Standards of Disclosure for Mineral Projects). Mr. Keating is the President, CEO and a Director of PJX.

THIS IS NOT AN OFFER OR SOLICITATION FOR THE PLACEMENT OF SECURITIES.

Disclaimer

Vine Property Highlights

Opportunity

• Historical Mining Area
• Existing Zinc-Lead-Silver Occurrences - not tested on strike
• Excellent Infrastructure - roads, power, rail
• Mining Friendly Communities - with experienced work force

Why hasn’t the area been fully explored?

• Fractionated Land Package - prevented concerted exploration

– PJX has consolidated the land and ownership

• New Exploration Technology - has identified large targets

PJX RESOURCES’ CRANBROOK AREA GOLD & BASE METAL PROPERTIES

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

• f the Sullivan Graben that

hosts the Sullivan Deposit.

• Sullivan Deposit was a Sedex

(Sedimentary Exhalative) style deposit . (160 million tonnes 5.86% zinc, 6.08% lead, 67 g/t silver).

• Sullivan Mine operated for 90

years & produced concentrate with a metal content equivalent to over $38 billion using today’s metal prices.

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

• rder basin.
• Faults act as a pathway for

fluids to descend to depth.

• Fluids are heated at depth and

leach zinc, lead, silver and other elements.

• Hot fluids with metals rise

along growth faults, breccias and feeder pipes forming a Vent Complex.

• Zinc, lead and silver form

sulphide minerals that deposit

• n the ocean floor as exhalative
• re, or beneath the ocean floor

as replacement ore.

(Zinc, Lead, Silver) (Zinc, Lead, Silver)

Sullivan SEDEX Deposit – East-West Cross Section

(Geological Survey of Canada, Lydon, et al.)

• Bedded exhalative ores of

Sphalerite (zinc sulphide), Galena (lead sulphide with silver), Pyrrhotite (iron sulphide, sometimes magnetic), and Pyrite (iron sulphide), occur above Footwall Conglomerate (Vent - Feeder pipe).

• Gabbro is believed to have

intruded along a syn- sedimentary growth fault at a later date.

Massive Sulphides (lead, zinc, silver) Vent- Feeder Pipe Gabbro

Sullivan Basin - Schematic North South Cross Section (By A. Hagen, Cominco, 1983)

• Two Vents – Sullivan Vent and orebody on right and Stemwinder Vent on left.
• Stemwinder Vent may have produced an orebody that has since been removed by erosion.
• Two Vents are approximately 2.5 km apart.
• Similar spatial relationship occurs for the Fors and Smoker Vents on PJX’s West Basin Property.

Vine & West Basin Properties

• Vine Vein - Historical resource

estimate (Non NI 43-101 Compliant) 1,300,000 tonnes grading 2.2 g/t gold, 36.3 g/t silver, 3.12% lead, 3.12% zinc and 0.11% copper (*Kokanee Exploration Ltd. Prospectus (1990)).

• Fors – Vent Complex with Sedex zinc-

lead-silver massive sulphide discovery.

• Smoker – Vent Breccia with zinc and

lead mineralization, 100m X 400m in surface area. If the vent produced a massive sulphide orebody then it may have been removed by erosion.

• Vine Property may have two vents

defined by gravity anomalies.

*Kokanee Exploration Ltd.’s resource estimate quoted above is a historical estimate and not prepared using the resource categorizations set out in NI 43-101. PJX is not aware of any more recent resource estimate for this

• property. PJX is uncertain as to the relevance or reliability of the historical estimate. PJX is not treating the

historical estimate as current mineral resources or reserves, as a qualified person has not done sufficient work to classify the historical estimate.

Vine Vein Structure at Surface

• Two historical drill holes (1990’s) are reported to have intersected Sedex style massive sulphides, approximately

300 metres below the Sullivan deposit time horizon, at the base of the footwall quartzite (approximately 700 metres down hole). – KV90-41 intersected 3.6 metres of 4.34% lead, 2.08% zinc, 42 g/t silver, 0.11 g/t gold, 0.41% copper – KV94-57 intersected 0.5 metres of 5.20% lead, 4.40% zinc, 41 g/t silver

(Note: drill hole data is historic and should be considered with caution as PJX is uncertain as to the relevance or reliability of the data)

Vine Property Large Eastern and Western Gravity Anomalies

• Massive sulphide mineralization

containing zinc, lead, silver and iron sulphides are often more dense than surrounding rocks and this density contrast can appear as a positive gravity anomaly (red areas on gravity map).

• Historical drill holes (1990 and

1994) intersected massive sulphide (zinc,lead,silver) mineralization on what appears to be the western edge of the eastern gravity target area.

• This slide displays gravity from 5

km’s deep to surface. The next slide displays gravity from 1.2 km’s deep to surface and defines what may be a 3rd order basin.

Hole VA15-02 intersected a possible restricted 3rd order sedimentary basin that may be similar to the geological environment often associated with Sedex massive sulphide deposits containing zinc- lead-silver.

Gravity anomaly associated with possible 3rd order basin

Cross Section WW

Vine Property - Interpreted Geological Cross Section WW

• 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).

• PJX hole VA15-02 intersected what appears to be a thick gabbro sill before entering Lower Aldridge (LA) sediments that contain anomalous

sphalerite (zinc mineralization) and alteration (sericite, chlorite, albite) in some sedimentary beds.

• The company believes that the thick gabbro sill defines a possible 3rd Order Sedimentary Basin. Massive Sulphide deposits often occur in 3rd
• rder basins.
• The base of the FWQ horizon in the basin is considered to be at depth below hole VA15-02, and is a target for the next phase of drilling.
• Hole VA15-02 also encountered folded deformed rocks (DP Zone) that contain sphalerite. This zone could host a folded and thickened

massive sulphide body (see conceptual interpretation on section) and is also a target for the next phase of drilling.

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 located within a few kilometres of the target areas.

• CPR Rail line was used to transport zinc-

lead-silver concentrate from the Sullivan Mine (North of Cranbrook) through the Vine Property to Teck’s (Cominco) Smelter Complex in Trail, British Columbia.

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 other markets.

Vine Property

Directors’ and Officers’ Biographies

• John Keating, PGeo – Chief Executive Officer, President and Director
• Mr. Keating has over 30 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, silver, and base metals with the Federal Government of

• Canada. During the last 10 years, Mr. Keating was President and Chief Executive Officer for Black Bull Resources and Golden Chalice
• Resources. Mr. Keating holds a BSc(Geology) from Concordia University, Montreal, Quebec.
• Linda Brennan – Chief Financial Officer, Corporate Secretary and Director
• Ms. Brennan has been a consultant for 12 years providing strategic advice and organizing and structuring financings to numerous

early stage companies in the junior resource sector. She brings knowledge of finance, accounting and public markets to PJX. She has also served in the capacity of corporate secretary for several TSXV listed companies. Ms. Brennan holds Business Administration and Bachelor of Commerce degrees from the University of Victoria and Royal Roads University, respectively.

• James Clare – Director
• Mr. Clare is a member of the Canadian Bar Association and a Partner with Bennett Jones LLP. Mr. Clare practices in the areas of

corporate and securities law, with an emphasis on corporate finance and mergers and acquisitions. Mr. Clare’s practice is focused on the mining and oil and gas sectors. His transactional experience includes domestic and cross-border public and private corporate finance transactions, representing issuers and agents as well as merger and acquisitions transactions. He also advises public issuers

• n general corporate and securities law matters including stock exchange listings, continuous disclosure obligations and other

regulatory compliance issues. Mr. Clare holds Bachelor of Laws and Bachelor of Arts degrees from the University of Western Ontario and Acadia University, respectively.

Directors’ and Officers’ Biographies

• Kent Pearson, PGeo – Director
• Mr. Pearson is a geologist with over 20 years experience in the mining and capital markets sectors. His background in mining includes

both exploration and production. His capital markets experience includes equity and debt research and investment banking as a vice

• president. He is currently president of Locarno Advisory Inc. a boutique advisory firm specializing in corporate mergers and

acquisitions, strategic advisory, asset review and asset disposition. Mr. Pearson holds a BSc (Geology) from the University of Alberta. In addition, he has earned a MBA from Queen’s University, Kingston, Ontario.

• Somerset Parker - Director
• Mr. Parker is currently the Vice President, Marketing Division of Geovic Mining Corporation. Mr. Parker previously held a senior

management role at Jaguar Nickel Inc. As Director of Marketing and Sales for Falconbridge Limited, Mr. Parker negotiated and managed contracts and sales for Falconbridge products in Latin America, Asia, Europe and Canada during his 14 years with the company, beginning in 1981. Mr. Parker has developed an extensive network of investor contacts and mining analysts, on a worldwide basis, including relationships with major banks and securities houses. Mr. Parker holds a Bachelor of Science, University

• f Chile.
• Joseph Del Campo – Director
• Mr. Del Campo holds a Certified Management Accountant designation. Mr. Del Campo worked for the Falconbridge group of

companies in financial positions, including Controller and Treasurer of Falconbridge Dominicana and Falconbridge Gold Corporation, a gold mining company with operating mines in Africa and Canada. Over the past 13 years, Mr. Del Campo has been a director and vice president of finance and chief executive officer at a number of junior exploration companies listed on the TSX and TSXV and is the former CFO of First Nickel Inc.

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 expertise spans most metallic deposit types including :

• 1. Sedex deposits in the Purcell Supergroup of Canada where he co-edited and authored several papers in the major treatise
• n the Sullivan deposit , titled “The Geological Environment of the Sullivan deposit”;
• 2. Silver vein deposits in the Slocan Silver camp, British Columbia.
• 3. Copper-gold vein, porphyry, and skarn type deposits in British Columbia, the Yukon Territory, and Mexico.
• 4. Gold vein and epithermal gold deposits in British Columbia and Mexico

David (Dave) Leo Pighin , P.Geo

• Mr. Pighin is a Professional Geologist with over 45 years of mineral exploration experience . During his 24 years with Cominco Ltd.,

Dave was involved with mapping local and regional geology at the Sullivan Mine and was also involved with the development and use

• f the Aldridge Marker Bed Horizons as a proven exploration tool. Dave discovered the Fors zinc-lead-silver Sedex massive sulphide
• ccurrence in 1966 and the Vine zinc-lead-silver-gold vein deposit in 1976 with Cominco. He has since designed and managed

programs ranging from grass roots exploration to advanced drilling for gold, silver, diamonds, rare earths, gypsum, and base metals, mainly in the Province of BC, and also in the Yukon, Northwest Territories, Western U.S.A., and Mexico.

PJX Capital Structure

Listed on TSX Venture Exchange (PJX.V) Share Structure Current as of August 2015 Shares Issued: 50,178,446 Warrants: 24,840,245 Options: 4,867,000

Investment Highlights and Next Steps

– PJX is focused on building shareholder value and community opportunity through the exploration and development of mineral resources with a focus on gold, silver and base metals (zinc, lead, copper). – Experienced Management team, Consultants and Board with over 200 years of cumulative experience in the exploration and mining industry. – Current exploration is primarily focused on the Vine Property. PJX owns mineral title to the Vine Property, subject to a 1% NSR

• n part of the property.

– Geological environment is favourable to discover Sedimentary Exhalative (Sedex) zinc, lead, silver massive sulphide deposits. – The Sullivan Sedex deposit, located 35km north of the Vine Property, occurs in a 3rd order sedimentary basin and operated for

• ver 90 years and produced about 8 million tonnes of zinc, 9 million tonnes of lead, and 285 million ounces of silver, equivalent

in value to over $38 billion using today’s metal prices. – Two target areas have been identified by geophysics for testing on the Vine Property. Recent hole VA15-02 has intersected a possible 3rd order sedimentary basin that could host a massive sulphide deposit. – The Vine Property is road accessible year round and close to power, rail, and mining friendly communities of Cranbrook and Kimberley, British Columbia, Canada. – Some of the world’s largest zinc, lead and silver mines closed, or are closing, due to ore reserve depletion, such as the Brunswick Mine in New Brunswick, the Century deposit in Australia, the Main deposit at Red Dog in Alaska. – Next Steps - detailed gravity has defined a large target to test by drilling.

For Additional Information Contact: PJX Resources Inc. 5600 – 100 King Street West Toronto Ontario M5X 1C9 416-799-9205 info@pjxresources.com Attention: Linda Brennan

• r visit our web site at:

www.pjxresources.com