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Lake Winn Announces Completion of 3D Model of Pegmatite Dykes at Little Nahanni Lithium Project, Northwest Territories, Canada
(TheNewswire) June 21 st , 2023 – Vancouver, British Columbia – L...
About this update from Lake Winn Resources Corp.
[{"type":"text","content":"Lake Winn Announces Completion of 3D Model of Pegmatite Dykes at Little Nahanni Lithium Project, Northwest Territories, Canada\n \n \n (TheNewswire)\n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n June\n21\n \n \n st\n \n \n , 2023 – Vancouver,\nBritish Columbia – Lake Winn Resources Corp.\n \n \n (“\n \n \n Lake Winn\n \n \n ” or the “\n \n \n Company\n \n \n ”) (TSXV:LWR) (FSE:EE1A) is pleased\nto provide an update on recent activities related to its Little\nNahanni Lithium Project (“the Project”) located in western\nNorthwest Territories (NWT) as shown on Figure 1. The Project is 100%\nowned and covers 7,080 hectares of prospective ground.\n \n \n \n \n \n \n \n \n Click Image To View Full Size\n \n \n \n \n The Little Nahanni Lithium Project was modelled by\nArcher, Cathro & Associates (1981) Limited at the request of Lake\nWinn to better define the pegmatite swarms in 3D and to assist in\nfuture exploration efforts on the Project. Data to date is\ninsufficient to model for any purpose other than highlighting future\nexploration targets and trends.\n \n \n \n \n \n \n The prospect comprises a\nseries of dyke swarms which strike over 7,000 m along the extent of\nthe claim group. Swarms range from 50 m to 250 m in width, with\nindividual dykes typically 1-10 m wide. The dyke swarms dip steeply to\nthe north-east and have been demonstrated in outcrop and drilling to\nhave a vertical extent of 300 m or more.\n \n \n \n \n Modelling was performed in Seequent Leapfrog Geo using\nsurface mapping points and interpretations derived from previous\nexploration campaigns. Drill data, where possible,\n \n \n was incorporated in order to refine models and or add\npotential targets for further evaluation. Over 600 historical surface\nmapping points were used across the region to define the dyke swarms\nas well as model individual dykes. Classification and naming\nconventions were retained. Where local fault offsets were inferred\nfrom previous assessments, these were honoured as much as possible.\nDip orientations were derived from surface mapping and projected to\ndepth. The dykes remain open to depth and the full vertical extent of\nthe dykes is unknown. They are modelled to an arbitrary depth, but\nthis is not based on any cu...