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The Lingman Lake property possesses significant geological characteristics of gold environments that are common with contemporary models of Archean lode gold greenstone belts. Some of the more salient features include:
- Regional scale deformation zone.
- Gold enriched quartz veins and silicification alteration zones and shear zones.
- Multiple sub-parallel and branching shear zones over a wide area, extending along a strike length in excess of 1,000-meters and 260-meters in width.
- Multi-phase intrusions ranging from regional scale granitic terranes to property level feldspar ± quartz porphyry.
- Poly-sulphide mineralization that includes; pyrite, arsenopyrite, chalcopyrite, galena and sphalerite.
- Multi-environment gold mineral associations that include; gold in silicification zones, quartz veins and veinlets, in metavlocanic-intrusive contact proximal zones, and within intrusive rocks.
- Only 20% of the property (McPhee 1989) reported to have been subjected to detailed exploration.
- Bulk sample assay results significantly higher than core sample assays. Bulk samples averaged at 17.3 gpt (0.51 opt) versus McPhee average from drilling of 6.86 gpt (0.20 opt)!
- Depth potential illustrated by 1973 hole drilled to 302-meters (992-ft) intersecting the North Zone; returned an assay from 283.5-285.0-meters, (930.1-935.0 ft) a 1.5-meter (4.9 ft) interval grading 325.7 gpt gold (9.50 opt), (Crouse 1973)