Advance United Holdings Inc. and Frontline Gold Inc. reported numerous favorable geophysical anomalies have been identified on the Paint Lake Road JV (PLR JV) Property. The project is within the Wawa Abitibi Subprovince, prolifically known for its metal endowment. It has been estimated the Abitibi Subprovince has produced over 200 million ounces of gold and 400 million tonnes of base metal ore.

The belt has recently been consolidated and the Paint Lake Road property is strategically located inside the consolidated area near the Mishi Open Pit and the former Magnacon Mines. The property comprises six (6) claim blocks totaling over 3,610 hectares 50km north of Wawa, Ontario and is located inside the Mishibishu Greenstone Belt which hosts the Wesdome Mines, the Eagle River Gold Mine, the Mishi Open Pit, and the former Magnacon Mine. Advance United has had success in the Wawa area having formerly developed and sold the Dorset Zone to current owners, Angus Ventures, which hosts a non-compliant resource of 100,000 oz.

gold. The full story can be read here. The Paint Lake Road property sits along the Pukaskwa-Iron Lake (PIL) Shear Zone, known to host gold mineralization at the former Argo property and further south at Wesdome's Camp Lake occurrence.

Further northeast the Iron Lake Shear Zone hosts Alamos' Island Lake Mine. The Paint Lake Road Property Geology The Property occurs within the Mishibishu greenstone belt that is a broad arcuate syncline 55 km long east-west and 16 km wide north-south. This belt is part of the Wawa Subprovince of the Archean age Superior Province.

Supracrustal rocks in the belt are dominated by greenschist facies mafic to intermediate volcanic rocks with lesser sedimentary rocks including iron formation and intermediate to felsic volcanic rocks. The belt is surrounded by Archean granitic rocks and includes two internal granitic batholiths occupying the central portion of the belt. The northern limb of the belt, where the PLR JV Property and the Mishi Mine of Wesdome are located is dominated by an assemblage of clastic sedimentary rocks, felsic tuffs, and mafic flows.

The southern limb, where the Eagle River Mine is located, is dominated by tholeiitic basalts and calc-alkaline andesites with minor interflow clastic sedimentary rocks and lean chert-magnetite iron formation. Promising Paint Lake Road Targets: The target for exploration on the PLR JV is shear-hosted orogenic gold similar to Wesdome's Eagle Deposit which is hosted by quartz veins in shear zones hosted by intrusive diorite. The presence of a regional scale shear zone is considered prospective for this type of deposit.

Gold bearing quartz veins at Eagle River are hosted primarily by subvertical to steeply north dipping east-west striking shear zones within an elliptical quartz diorite stock Mineralized structures exhibit broad zones of deformed rock (3-20 m wide shear zones) affiliated with strong silicification over 20-50 m width. The PLR JV property is underlain by intrusive rocks and as such has been largely ignored in previous exploration programs. The identification of possible shear offsets from the main PIL shear will be further explored with prospecting and sampling.