Receives Tsxv Approval On The Advanced Kerrs Gold Deposit In Ontario’s Prolific Abitibi Greenstone Gold Belt
iMetal Resources Inc. (TSX.V: IMR) (OTCBB: ADTFF) (FRANKFURT: A7V2) is pleased to announce that it has received the approval of the TSX Venture Exchangefor the option to acquire 100% of the 665 hectare Kerrs Gold Deposit, located 90 kilometres east-northeast of Timmins, Ontario, in the Abitibi Greenstone Gold Belt.
The Kerrs Gold Deposit is comprised of a series of gold-bearing pyritized quartz vein replacement breccias enveloped by quartz fuchsite carbonate vein breccias averaging 10 metres in thickness. The deposit hosts a historical resource estimate of 7,041,460 tonnes grading 1.71 g/t gold yielding 386,467 ounces at a 0.5 g/t gold cut-off. Drilling subsequent to the historic estimate appears to have extended the mineralized zone along strike and down dip.
“The Kerrs Gold Deposit is the perfect complement to Gowganda West, giving iMetal multiple highly prospective projects in the prolific producing Abitibi Greenstone Gold Belt. The Company’s focus remains on closing its up-sized financing to fund sufficient diamond drilling to both bring the Kerrs 386,467 ounce historic resource current and build upon it, as well as undertake follow-up drilling at Gowganda West,” commented iMetal CEO Saf Dhillon. “The Company has come a long way under the new management team, continuing to build value for iMetal shareholders and we look forward to a successful 2022,” he concluded.
The Kerrs Gold historical resources estimate was disclosed in “NI 43-101 Resource Estimation on the Kerrs Gold Deposit, Matheson, Ontario” prepared for Sheltered Oak Resources Inc. by Garth Kirkham, P. Geo of Kirkham Geosystems Ltd., and dated June 10, 2011. The Company considers the resource estimate relevant as it will drive further exploration by the Company and reliable, as it was completed by a competent Qualified Person to the standards of the day. The resource estimation methods and parameters were as follows:
The Kerrs historic estimate is an inferred resource as defined in National Instrument 43-101. The Company is not aware of any more recent resource estimates, though there was further drilling completed after the historic estimate was released. The Company will need to review the historical drilling and analyses and will need to twin a number of the historic holes to bring the historic estimate current. The Company’s Qualified Person has not done sufficient work to classify the historic estimate as a current mineral resource. iMetal is not treating the historical estimate as a current mineral resource.
The Kerrs Gold Deposit
Figure 1. Kerrs Gold Deposit
The road accessible Kerrs Gold Deposit consists of 36 units totaling approximately 665 hectares and lies 90 kilometres east-northeast of Timmins, Ontario in the Abitibi Greenstone Gold Belt.
The Deposit was discovered by Noranda in the late 1970’s early 1980’s by following glacial dispersion trains up-ice to the source. Drilling continued into the late 1980’s, with further drilling in the early to late-2000’s and early 2011’s. The drilling database was used to calculate the 2011 historic resource estimate, with further drilling completed subsequent to the release of the estimate. The Kerrs Gold Deposit consists of a series of gold-bearing pyritized quartz vein replacement breccias enveloped by quartz fuchsite carbonate vein breccias averaging approximately 10 metres and alteration envelopes varying up to 40 metres in thickness. Gold is directly related to pyrite content which ranges to 10% and is commonly found as disseminations and crystal aggregates in the sheeted, quartz vein replacement breccias. These breccias, averaging 31% quartz, exhibit reasonable correlation conforming to volcano-stratigraphic contacts as well as moderate to good continuity in grade correlations at the lower and upper boundaries of the vein breccia and alteration envelope assemblages.
The Kerrs Gold Deposit is stratabound, occurring at the contact of a thick, mafic pillow flow sequence overlying an ultramafic, magnetite-rich flow sequence. Quartz feldspar porphyry sills are spatially located above and below the breccia zones. This stratigraphy is synclinally folded with the deposit lying 350 m to 425 m below surface. Drilling has traced the main zone 800 metres and remains open in both directions and at depth.
The Company continues to review the historical database to define target areas to both significantly expand the historic resource and to test for additional structures. The Company has yet to verify the historical data.
The Kerrs Agreement
iMetal entered into a purchase option agreement (the “Option Agreement”), dated January 24th, 2022, with Gravel Ridge Resources Ltd. and 1544230 Ontario Inc. (collectively, the “Vendors”) pursuant to which was granted the right to acquire the Kerrs Gold Deposit.
To acquire the Deposit, the Company is required to issue 3,500,000 common shares (the “Consideration Shares”) and complete a series of four cash payments totaling $210,000 to the Vendors as follows:
Following completion of the above cash payments and share issuances, the Company will acquire the Deposit and will grant to the Vendors a three percent royalty (the “Royalty”) on net smelter returns from the Deposit. The Company may acquire two percent of the Royalty from the Vendors at any time by completing a one-time cash payment of $2,000,000.
The Company is at arms-length from each of the Vendors. No finders’ fees or commissions are payable in connection with the Option Agreement. The Consideration Shares are subject to a statutory hold period until August 2, 2022, in accordance with applicable securities laws.
The scientific and technical information contained in this news release has been reviewed and approved by R. Tim Henneberry, P.Geo (British Columbia), a director of iMetal and a qualified person as defined in National Instrument 43-101.
Disclaimer iMetal is a paid marketing client*