©
Copyright 2004 by Strongbow Exploration Inc. All rights reserved.
www.strongbowexploration.com
Strongbow’s
100% owned Anialik and Rush properties comprise 55,850 ha of Inuit Owned Lands
subject to the
NTI Agreement covering the Anialik River volcanic belt (ARVB)
in the northern Archean Slave Structural Province. The ARVB is one of the few
remaining under explored greenstone belts in Canada. The northern part of the
belt is on tide water at Coronation Gulf. A number of gold and base metal showings
have been identified, including the Run Lake VMS deposit that has been tested
by 48 of the 66 reported drill holes within the property. A number of gold
showings were ground checked by Strongbow in 2003 and selective sampling confirmed
elevated gold values in the range of 20-50 g/t, with the highest grade surface
grab sample returning 799 g/t gold from the Wolf showing in the northwest part
of the property. Earlier workers have also identified 2 mineralized boulders
(15.2 g/t Au, 150 g/t Ag, 8.6% Cu; and 164 g/t Ag, 10.3% Cu) in the north central
part of the Anialik belt and Strongbow recently (Spring 2004) completed a detailed
helicopter borne magnetic and electromagnetic survey over intermediate to felsic
volcanic rocks located up ice from these boulders.
The Rush property is located just east of the ARVB, approximately 7km west of
Wolfden Resources High Lake VMS deposit (5.3 million tones averaging 4.0% copper,
2.4% zinc, 1.8 g/t Au, and 32 g/t Ag). Proximity and similar geological setting
to the High Lake deposit are motivating factors for Strongbow to explore for
similar style polymetallic VMS mineralization on the Rush and Anialik properties.
Despite its proximity to the High Lake deposit, past exploration of the Rush
property area has been very limited, with only a single drill hole reported within
the property boundary. Three areas of base metal mineralization have been identified
by earlier workers as well as significant alteration zones potentially indicative
of VMS style mineralization.
Geophysical data collected over the Rush and Anialik properties have been interpreted
and follow up prospecting and mapping was conducted during July and August, 2004.
Results of this work are currently being received and will be used to identify
target areas for follow up work in 2005.