WINDFALL

Despite the lack of outcrops in the southern part of the property, Goutier has determined that the heart of the property is occupied by the imbricated structure of the Malartic-Kinojevis groups, between the Aiguebelle and La pause fault zones, which is similar to a tectonic front associated with overlapping formations having a northern direction. This is a very complex area, both relative to the number of overlaps and faults. We find a sequence of overlapping panels of basalt-komatiite and rhyolite-turbidite, a multitude of syn-tectonic dykes and volcanics from the Malartic formation.

The Destorbelle Showing is located within a sequence of ultramafic volcanic rocks, steeply dipping, weakly to moderately sheared and deformed. The mineralized zone is spatially associated with brecciated and altered ultramafic and a graphitic tectonic breccia. Breccia horizons are oriented EW to WNW-ESE and dips steeply to the S-SW.