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The Snowbird Nickel project consists of approximately 900,000 acres of mineral claims and permits located along a 240 km strike length of the southern Snowbird Tectonic Zone (SBTZ). The SBTZ is a major crustal scale structure that represents an underexplored region prospective for magmatic sulphide nickel deposits. This northeast-trending structure can be traced for over 2,800 km from the Rocky Mountains to Hudson Bay. There is evidence from regional geological and geophysical datasets that, in the area of Strongbow's properties, the SBTZ has been intruded by numerous mafic-ultramafic rocks. Some of these intrusions are known to host nickel-copper sulphide mineralization, including the mineralized zones currently being drilled at Strongbow's Nickel King property.
In May 2007 the Company completed airborne magnetic and electromagnetic surveys over portions of the Snowbird Nickel project. In March of 2008 a detailed Versatile Time Domain Electromagnetic (VTEM) survey was completed over five areas within the project area. In addition to these airborne surveys extensive mapping, prospecting and sampling programs have been completed during the 2007 and 2008 field seasons. Currently there are eight priority target areas within the Snowbird Nickel project.
Reeve Lake, SK --
• 25 km north of Stony Rapids;
• VTEM survey produced eight modeled responses in association with magnetic highs;
• Prospecting samples returned from background to 0.13% Ni and 0.11% Cu from a gabbroic intrusion;
• Way Forward -- detailed ground program involving prospecting and mapping, ground geophysics to define drilling targets from modeled airborne anomalies, and drilling.
Nickel Lake, SK --
• 30 km north of Stony Rapids;
• ~650 m coincident magnetic/electromagnetic anomaly;
• Prospecting samples returned from background to 0.45% Ni and 0.15% Cu from a norite intrusion;
• 2008 drilling (1 hole, 249 m) returned 1.9% Ni, 0.96% Cu and 0.11% Co over 0.80 m;
• Way Forward -- down hole geophysics, and additional drilling to test the extent of mineralization.
Dumas Lake, SK --
• 40 km northeast of Stony Rapids
• 4,400 m discontinuous, coincident magnetic/electromagnetic anomaly that is spatially related to norite sills intersected in 2008 drilling; VTEM survey produced 18 modeled responses;
• Mineralization identified at shallow levels (<75 m depth) in 4 zones over a 2,000 m strike length;
• Historically best drill intercepts include 2 m grading 1.36% Ni and 0.94% Cu (Zone A) and 0.5 m grading 2.36% Ni (Zone D);
• Modeling suggesting airborne conductors are strongest at depths of 100-150 m and that the strongest conductor is located at the western end of the trend, approximately 1,000 m west of the historic exploration work;
• 2008 drilling program (771.5 m; 5 drill holes) tested historic and new targets; best results seen in DS08-003 with 0.88% Ni, 0.51% Cu and 0.04% Co over 0.55 m;
• Way Forward -- surface geophysics to better define airborne anomalies, down hole geophysics to vector mineralization, continuation of detailed mapping and surface sampling, and drilling.
Five Mile, SK --
• 48 km north-east of Stony Rapids;
• 4 km long magnetic trend with strong correlation to three discontinuous electromagnetic responses;
• Prospecting identified limited exposure of weakly mineralized mafic units;
• Initial indications for PGE mineralization in addition to anomalous Ni and Cu values from prospecting samples;
• Way Forward - detailed mapping, soil and biogeochemical sampling and prospecting focusing on identifying additional mafic units.
Breynat Lake, SK --
• 80 km north of Stony Rapids;
• Extensive area mafic intrusive rocks mapped by previous workers;
• 1,200 m long coincident magnetic/electromagnetic anomaly; 9 electromagnetic responses modeled from VTEM airborn survey;
• Way Forward - detailed mapping, soil and biogeochemical sampling and prospecting focusing on modeled electromagnetic responses.
Heel, SK --
• Located 70 km Northeast of Stony Rapids and 65 Km southwest of Nickel King;
• Coincident magnetic/electromagnetic anomalies; detailed VTEM survey returned 17 modeled plates;
• Anomalous Ni, Cu, Co lake sediment, soil-biogeochemical geochemistry;
• 2008 surface prospecting and mapping identified several localities with gabbroic units which have returned values ranging from background to 0.46% Ni and background to 0.57% Cu;
• Initial indications for PGE mineralization in addition to anomalous Ni and Cu values from prospecting samples;
• Way Forward - additional mapping, detailed work on extending showings, and defining drilling targets.
Opescal Lake, SK/NWT --
• Straddles the SK/NWT border approximately 30 km southwest of Nickel King;
• Numerous coincident late channel EM and magnetic anomalies; modeling of detailed VTEM survey returned 30 electromagnetic conductors;
• Ground follow up has identified mafic and ultramafic intrusive rocks with MgO contents locally in excess of 30%;
• Anomalous Ni, Cu, Co lake sediment, soil-biogeochemical geochemistry;
• Prospecting samples returned from background to 0.26% Ni, 0.30% Cu, 0.83 g/t Pd and 0.84 g/t Pt;
• Mapping of the area identified several thin mafic units in association with electromagnetic conductors;
• Way Forward - detailed mapping and prospecting, ground geophysics, defining drilling program.
Wholdaia Lake, NWT --
• 50 km north of Nickel King, 185 km northeast of Stony Rapids;
• Several electromagnetic anomalies require further evaluation;
• Same geological setting as Nickel King (paragneiss / orthogniess rocks of the Rae Province);
• Way Forward - detailed prospecting, mapping and soil-biogeochemical sampling.
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