Meridius Options Dunlop Bay Property in Matagami Mining Camp, Quebec and Appoints New CEO

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Vancouver, British Columbia--(Newsfile Corp. - August 21, 2020) -  Meridius Resources Limited (TSXV: MRI) (FSE: 8M0) ("Meridius" or the "Company") is pleased to announce that that it is expanding its acquisitions by reaching an agreement to option ( the "Option Agreement") the Dunlop Bay Property ( "Dunlop Bay" or the "Property"), located in the Matagami region in the Province of Quebec. Under the Option Agreement, Meridius has the right to acquire 100% ownership in 76 mineral claims that cover 4,226 hectares.

The Property is located immediately north of the Matagami Gold and Base Metals District, 15 km north-east from Glencore's Matagami Lake Mine Plant, processing zinc, copper, silver and gold material from the Bracemac-McLoed Mine. (see map 1) The Matagami camp has produced over 4.6 Mt of zinc, and 0.49 Mt of copper in addition to silver and gold from more than 63 Mt of ore1 between 1960 and 2004.2 Reader are cautioned that mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of the mineralization hosted on the Company's property.



Map 1: Geological map of the Dunlop Bay property in relation past and present gold producing mines.

To view an enhanced version of Map 1, please visit:
https://orders.newsfilecorp.com/files/5785/62243_f0c1d48f34099ac6_009full.jpg

The Dunlop Bay property, optioned by Meridius, hosts the main occurrence of gold mineralization in the Matagami district. Regionally, the property is located on the eastern extension of the Detour-Grasset deformation corridor, known for its gold endowment. The Wallbridge's Fenelon project is located 75km north-west of the Dunlop Bay project.

The Dunlop Bay gold system was discovered in the late 1950's by surface prospection and the property was further explored during the next four decades by ground trenching geophysics and drilling. More than 18,695 metres of drilling distributed in 114 holes was conducted between 1985 and 1995 on the main gold occurrence, intersecting a series of quartz veins, veinlets, and breccia varying from a few centimeters to up to one metre in width. The vein network can be followed along a strike for 700 metres, tested at depth to about 200 metres. Historical results are in the range of 3 g/t to 20 g/t over 0.3 to 1.3 metres from individual veins.3 Gold bearing quartz veins and fracture networks are distributed at short range from the contact of the Dunlop Bay intrusion, inside a magnetic halo. Elsewhere in the Abitibi Greenstone Belt, these types of intrusions, commonly identified as Syenite, offer favorable geological conditions for the deposition of gold.