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Location: 29 km NW from Schefferville, Quebec, Canada
83 & 85 AtlanticScheffervilleQuebec, CanadaG0G 2T0
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The LabMag Property is located in the western margin of the Labrador Trough, adjacent to Archean basement gneisses. The Labrador Trough, also known as the LabradorQuebec Fold Belt, extends for more than 1,000 km along the eastern margin of the Superior Craton, from Ungava Bay to Lac Pletipi in Quebec. The belt is about 100 km wide in its central part and narrows considerably to the north and south. The Grenville Front crosses the southern part of the Labrador Trough.The Deposit consists of magnetite Banded Iron Formation (“BIF”) of the Lake Superior type. BIFs are sedimentary rocks composed of alternating mm- to cm-scale beds of quartz (chert or jasper) and iron oxides (predominantly magnetite and hematite).The taconite at LabMag consists mostly of alternating small-scale (mm to cm) beds ofrecrystallized chert or jasper and massive or disseminated magnetite. Magnetite is the predominant iron oxide mineral, while hematite and martite occur in subordinate amounts. Gangue minerals are represented by iron silicates (minnesotaite and stilpnomelane), iron carbonate (siderite) and manganese carbonates (rhodochrosite and kutnahorite).This iron formation has been explored by diamond drilling over a strike length of 9.5 km (Blocks A, B and C) and it extends beyond the northwest and southeast Property boundaries.
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