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Goldstrike Drilling Update-Visible Gold Intersected in Three Holes at Plateau South

VANCOUVER, BRITISH COLUMBIA--(Marketwired - July 15, 2013) - Goldstrike Resources Ltd. (TSX VENTURE:GSR)(APRAF)(KCG1.F) is pleased to report that early exploratory drilling at the VG Zone on its flagship 100% owned Plateau South property in Eastern Yukon has intersected mineralization with visible gold in three of the first six holes (PSVG13-02, PSVG03, PSVG-06), and sulphide mineralization in every hole drilled to date, and the zone remains open. PSVG13-06 was drilled on trend 32 metres southwest of Hole PSVG13-03, and 20 metres southwest of Hole PSVG13-02. All holes have targeted locations where visible gold and gold mineralization were previously discovered in surface felsenmeer confirmed to be two to five metres thick. The gold-bearing structure strikes northeast-southwest, and cuts a 25 metre layer (true thickness) of intensely quartz-flooded and albitized rhyolite volcanics. Some drill holes contain multiple mineralized quartz stockworks and veins up to three metres in true thickness. Based on these initial results, the 2013 drilling program has been expanded and is ongoing.

Different styles of mineralization discovered to date across the Gold Dome are associated with intense quartz flooding and bleaching, veining, stockworks, and brecciation. Free crystalline and wire gold occur alone or are associated with disseminated arsenopyrite and pyrite.

The Plateau South property covers the 25 kilometre long Yellow Giant Trend discovered by Goldstrike in 2012 - a regional scale, gold bearing deformation system and felsic volcanic complex where numerous high grade grab samples, including one returning 15.45 ounces of gold per ton (529.86 grams per tonne gold), have been documented in bedrock and subcrop in multiple zones of mineralization (News Release October 30, 2012).

Detailed geophysics shows that the VG Zone is located within part of a magnetic low trend about 1,200 metres long and 300 metres wide that remains open. This zone strikes obliquely across a broad flat-topped ridge measuring approximately 2 by 1 kilometres that is now referred to as the "Gold Dome". The magnetic low trend is associated with the intense silica and albite alteration of the host volcanics described above. Within the magnetic low trend the gold mineralization appears to be controlled by a grid of subvertical east-northeast fractures and west-northwest structures, both of which are thought to be related to an episode of northeast-directed thrust faulting and associated folding. Careful prospecting along several of the other geophysically indicated structures has already resulted in the discovery of numerous additional rock grab samples containing visible gold and/or sulphide minerals in silicified volcanic subcrop. Prospecting, mapping, and drilling are ongoing within the Gold Dome area, and all zones currently remain open.