TORONTO, April 21 /CNW/ - Nuinsco Resources Limited (NWI:TSX) announces today that it has commenced exploration on the Diabase Peninsula uranium property located in the Athabasca Basin of northern Saskatchewan. Nuinsco holds the property under option from Trend Mining Company of Denver, Colorado. A geophysical crew was mobilized to the property and has now completed a Transient EM survey on a grid established over the central part of the claim group. Approximately 68km of grid line has been surveyed using 800m by 600m loops. The survey was designed to trace and define geophysical conductors known to underlie the Diabase Peninsula Property at depths of 150-400m beneath the sediments of the Athabasca Basin. Electromagnetic surveys are used to identify buried unconformity related uranium mineralization in the Athabasca Basin - the survey identifies the presence of graphitic units, which provide a favourable environment for uranium deposits. Results of the survey will be reported when received by the Company. Subsequently Nuinsco expects to have the entire property covered by an airborne EM survey by early summer. The survey will extend geophysical coverage over favourable structures, such as the Cable Bay Shear Zone, known to underlie the claim group in a northeast direction. Little work has been conducted along this structure away from the historic surveys that date from the 1970s and early 1980s. The Diabase Peninsula Property currently consists of eight claims encompassing 21,040ha. Historic work has established the presence of highly prospective alteration and geophysical signatures underlying the claim group. The historic geophysical signatures are being targeted by the current survey in order to define targets for a diamond drilling program contemplated for later this year. The Diabase Peninsula Property is located on the western shore of Cree Lake approximately five kilometres north of the southern boundary of the Athabasca Basin. The claim group overlies the contact of the Mudjatik and Virgin River Domains which is occupied by the graphite-bearing Cable Bay Shear Zone - this structure is considered to be an important locus for uranium mineralization in this part of the Athabasca Basin. The claim group is known to encompass hydrothermally altered sandstone boulders and is underlain by electromagnetic geophysical anomalies indicating the possible presence of graphitic conductors in the basement. The hydrothermal alteration and the geophysical anomalies are considered to be diagnostic indicators of potential uranium mineralization. FORWARD-LOOKING STATEMENTS: Except for statements of historical fact, all statements in this news release - including, without limitation, statements regarding future plans and objectives of are forward-looking statements that involve various risks and uncertainties. There can be no assurance that such statements will prove to be accurate; actual results and future events could differ materially from those anticipated in such statements.
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