Gitennes Exploration Inc. - Rare Earths, Niobium and Tantalum at Blue Ice

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[{"type":"text","content":"\n\n\n Mar. 29, 2011 (Canada NewsWire Group) -- \n\n#ReleaseContent TABLE\n{\n BORDER-COLLAPSE: collapse\n}\nTR.cnwUnderlinedCell TD\n{\n BORDER-BOTTOM: #000000 1px solid\n}\nTR.cnwDoubleUnderlinedCell TD\n{\n BORDER-BOTTOM: #000000 3px double\n}\nTR.cnwBoldUnderlinedCell TD\n{\n BORDER-BOTTOM: #000000 3px solid\n}\nTD.cnwUnderlinedCell\n{\n BORDER-BOTTOM: #000000 1px solid\n}\nTD.cnwDoubleUnderlinedCell\n{\n BORDER-BOTTOM: #000000 3px double\n}\nTD.cnwBoldUnderlinedCell\n{\n BORDER-BOTTOM: #000000 3px solid\n}\n#ReleaseContent TABLE.cnwBorderedTable TD\n{\n BORDER-RIGHT: black 1px solid;\n PADDING-RIGHT: 2px;\n BORDER-TOP: black 1px solid;\n PADDING-LEFT: 2px;\n PADDING-BOTTOM: 2px;\n BORDER-LEFT: black 1px solid;\n PADDING-TOP: 2px;\n BORDER-BOTTOM: black 1px solid;\n BORDER-COLLAPSE: collapse\n}\n#ReleaseContent TABLE TD\n{\n PADDING-RIGHT: 2px;\n PADDING-LEFT: 2px;\n PADDING-BOTTOM: 2px;\n PADDING-TOP: 2px\n}\n\nVANCOUVER, March 29 /CNW/ - Gitennes Exploration Inc. (TSXV: GIT) is pleased to advise shareholders that rare earths, niobium and tantalum occur at the Blue Ice property. These rock samples were collected from outcrop during a late-2010 field programme, are selective grabs weighing 300 to 360 grams and are not representative of geological widths or structures. The host pegmatite dykes are very coarse-grained and much larger samples may be required to accurately determine rare element concentrations and grades.\n\n\n >\n\nAll values are reported in ppm (parts per million) and were determined by Acme Analytical Laboratories (Vancouver) Ltd. using a lithium borate fusion followed by ICP-MS analysis.\nResults to date are encouraging with a tendency to heavy rare earths dominating over light, as noted particularly in sample 31788 where total HREE exceed 7,000 ppm compared to LREE of 3,200 ppm. Three swarms of east-striking pegmatite have been mapped thus far at Blue Ice along a 1200 metre-long north-south corridor. Results reported here are from two separate pegmatite dykes 640 metres apart within a swarm of similar appearing dykes. Brown to black lustrous prismatic minerals are present in samples 24087 and 31788. Sample 31789 is from the same pegmatite body as 31788, had no obvious suspect minerals, instead being from a zone of intense alteration marked by grey mica, clay and quartz.\nThe Blue Ice property covers a large...

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