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NI 43-101

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NI 43-101

Mt Milligan North NI 43-101 Compliant Report

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RECENT NEWS

Doubleview Announces Appointment of New Chief Financial Officer July 20, 2017
Doubleview Announces Resignation of Director and Officer July 13, 2017
Doubleview retains Venture Liquidity Partners as market maker July 4, 2017
New Zinc-Silver Zone at Red Spring, soil sampled as high as 1.55% Zinc, 7.94 oz/t Silver and 3.89% Copper June 15, 2017
Doubleview Receives “DTC” Eligibility, and Amended Hat Exploration Permit June 5, 2017

Stock Quote

Symbole	dbv.v (TSX Venture)
Last Trade	0.05
Change	+0.00
Date	7/20/2017
Time	2:00pm
Open	0.05
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Volume	3600

Porphyry Deposits 101

Porphyry copper-gold deposits form in a variety of volcanic environments, most commonly in continental margins and intra-oceanic arcs. These are large scale magmatic-hydrothermal systems associated with a series of porphyritic intrusions, which result in extensive alteration footprints that we map and model to target high grade copper-gold mineralization. As in Ridgway Australia (Wilson et al 2003) and Red Chris in Canada (Norris, 2012) , the Hat porphyry deposits form in

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Gold Weight of Hat Deposit

Gold in Porphyry Deposits: Porphyry Deposits are defined as large tonnage mineral deposits with, variously, valuable amounts of copper, molybdenum, gold and silver and combinations of one or more of those metals. Related metals may include iron (magnetite), titanium, rhenium and zinc. For discussion purposes deposits are further defined as alkalic and calc-alkalic, each of which has distinctly different characteristics; a few deposits have aspects of both. Alkalic porphyries usually

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