Virginia Mines Inc. (?Virginia?) is pleased to announce that it has entered into an agreement with Anglo American, whereby Virginia transfers to Anglo American a 50 per cent undivided interest in the 469 mining claims comprising the Ashuanipi property, which covers 23,884 hectares and is situated south-east of the Caniapiscau reservoir, in the James Bay territory, province of Quebec. Anglo American must fund an aggregate of $5,000,000 in expenditures over a five-year period to maintain its 50 per cent undivided interest in the Ashuanipi property. Anglo American may, at its sole discretion, accelerate such funding. Virginia will be the operator during that period. Ashuanipi Property The Ashuanipi property lies within the Caniapiscau lithotectonic division of the Ashuanipi high metamorphic-plutonic complex. The Caniapiscau domain is distinguished from other divisions of the Ashuanipi Complex by the presence of large, well-preserved volcano-sedimentary sequences and by the lower grade metamorphic facies (amphibolite). The Caniapiscau division is bounded by major ENE-trending regional ?graben-like? or thrust faults, which could explain the better degree of preservation and the lower grade metamorphism of the Caniapiscau division compared to the rest of the Ashuanipi complex. The supracrustal sequences of the Caniapiscau domain are composed mostly of amphibolitic basalts locally injected by gabbroic sills. These units are inter-layered with felsic metavolcanic rocks and paragneiss. Syn-volcanic to syn-tectonic intrusions (diorite, quartz diorite, tonalite and monzogranite) are emplaced at the margins of the volcano-sedimentary belts. Limited reconnaissance programs carried out by Virginia between 2007 and 2011 identified several significant showings forming a major mineralized trend that extends for more than 8 kilometres on the south block of claims of the Ashuanipi property. These mineralized occurrences can be classified into two categories: (1) Au-Cu-Mo-Ag showings (disseminated chalcopyrite (1-15%), molybdenite (1-10%) and pyrite, within a granodioritic gneissic intrusive at the margin of the volcano-sedimentary belt. These Au-Cu-Mo-Ag mineralized zones returned values of up to 3.8 g/t Au, 49.6 g/t Ag, 8.6% Cu, and 1.3% Mo in selected samples and up to 1.93 g/t Au, 11.3 g/t Ag and 1.56% Cu over 3 metres including 4.36 g/t Au, 20.1 g/t Ag and 3.0% Cu over 1 metre in channel samples. (2) Cu-Zn-Au-Ag showings (disseminated to semi-massive pyrrhotite-pyrite ?sphalerite ?chalcopyrite ?galena) associated with strong hydrothermal alteration (quartz-tremolite ?phlogopite ?sericite ?muscovite) developed in volcanic units. These showings returned interesting values up to 6.29 g/t Au, 3.92% Cu, 8.94% Zn and 14.30 g/t Ag in selected grab samples and up to 3.78 g/t Au over 1 metre, and 1.30% Zn and 0.25 g/t Au over 2 metres in channel samples. This 8-kilometre-long mineralized trend is still almost untested and remains open at both ends. A major exploration program is scheduled in 2012 to evaluate the true potential of this newly-defined mineralized system. Historically ignored on the basis of its granulitic metamorphic facies, the Ashuanipi area proves to share textural, structural and lithological similarities with other high-grade metamorphic mineralized areas such as Chapada (Brazil) and Aitik (Sweden). www.angloamerican.com |