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Equitorial Exploration Announces Channel Sampling Results from the Li Lithium Property

(via Thenewswire.ca) Vancouver, BC, Canada / TheNewswire / September 6th, 2016 - Equ...

articleLake Winn Resources Corp.September 6, 20163/company/lake-winn-resources-corp/news/equitorial-exploration-announces-channel-sampling-results-from-the-li-lithium-property
Equitorial Exploration Announces Channel Sampling Results from the Li Lithium Property

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[{"type":"text","content":"Equitorial Exploration Announces Channel Sampling Results from the Li Lithium Property(via Thenewswire.ca)\n \n \nVancouver, BC, Canada / TheNewswire / September 6th, 2016 - Equitorial Exploration Corp. (the \"Company\") (TSX Venture Exchange: EXX, Frankfurt: EE1, US Pinksheet: EQTXF) (\"Equitorial\") is pleased to announce results from the 2016 exploration program on the Company's 100% owned Li lithium property which hosts the Little Nahanni pegmatite group (LNPG). The Li property lies 30 km northwest of the Cantung Mine Site in the Northwest Territories, immediately east of the Yukon Territory border (Figure 1). \n\n\n \nLithium-cesium-tantalum pegmatite dyke swarms on the Li property have been traced over a combined length of 13 km in mountainous terrain that is deeply incised by several east- or west-facing cirques. The sampled portions of the dyke swarms are up to 52.60 m wide. Each dyke swarm contains multiple dykes that range from 0.2 to 10 m in width. The dykes strike northerly and have near vertical dips. They are well exposed on cirque walls, but most of these areas are too steep to sample. Fortunately, relatively continuous bedrock exposures are accessible at the base of cliffs on the north and south side of cirques. Cirque floors are covered by overburden. \n\n\n \nDuring the 2016 field program, a total of 81 channel samples were cut across parts of the lithium-cesium-tantalum pegmatite dyke swarms that comprise the Prison Wall, Berlin Wall, Great Wall of China and Hadrian's Wall dyke swarms within cirques 3 and 4 (Figure 2). Highlights from individual dykes within and adjacent to dyke swarms include:\n\n\n \n\n\n-1.57 % Li2O, 250.3 g/t Ta2O5 and 0.95% SnO2 across 1.70 m;\n\n\n\n-2.04% Li2O, 57.8 g/t Ta2O5, 0.05% SnO2 across 4.00 m;\n\n\n\n-3.10% Li2O, 53.6 g/t Ta2O5, 0.03% SnO2 across 0.95 m;\n\n\n\n-2.33% Li2O, 59.0 g/t Ta2O5, 0.05% SnO2 across 1.20 m;\n\n\n\n-1.67% Li2O, 41.4 g/t Ta2O5, 0.03% SnO2 across 3.75 m;\n\n\n\n-1.83% Li2O, 67.3 g/t Ta2O5, 0.05% SnO2 across 1.25 m; and,\n\n\n\n-1.63% Li2O, 52.9 g/t Ta2O5, 0.01% SnO2 across 5.15 m.\n\n\n\n\n \nThe dykes are separated by sedimentary wallrocks including quartz sandstone, limestone and shale, which do not contain significant amounts of any elements of interest. When calculating weighted average grades for the dyke swarms, the wallrocks were assigned zero value...

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