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Crack Minesight 7.5
Dec 07, 2005 (B Nelson) - The Leitch Mine property lies within the southern portion of the Wabigoon Sub-province in the Beardmore Geraldton Belt. This belt is further sub-divided into the Southern Metavolcanic Sub-belt and the Southern Metasedimentary Sub-belt. It is within the latter that the property is situated. This sub-belt is primarily sedimentary rocks, but contains interfingerings of basic to intermediate volcanic rocks. 94% of the gold produced in the Beardmore-Geraldton camp is from the Southern Metasedimentary Sub-belt. East-trending iron formations, up to 244 m wide, occur in the sediments. A prominent flat-lying diabase sheet, dipping 10-15 degrees to the west was intersected in the Leitch No. 1 shaft. This 'sill' is interpreted to be the same unit that intersects the Northern Empire ore zone 7 km to the southeast. Isoclinal folding and tight drag folding in the Beardmore and Geraldton areas, specifically observable in the iron formation, appear necessary controls for ore structure developments. Drag folds and ore-bearing structures throughout the belt plunge westward at 35 to 40 degrees. Gold mineralization occurs in two sets of narrow quartz veins occupying fractures in the greywacke; those parallel to the fold axial plane in shear zones and those nearly perpendicular to the axial plane. These veins are strongly sheared, and contain transverse, healed, tension gashes. The depth continuity of the veins normally exceeds the horizontal continuity by a multiple of 15. The veins range in width from 10 cm to 45.7 cm on avg., and many parts of the veins are contorted with thickened portions in the bends of folds. They consist mainly of light grey to white quartz with common chlorite-sericite banding parallel to the walls, representing a 'crack-seal' texture. Five veins have been mined. They are located on the flank of an anticline which apparently controlled their strike, dip and plunge (50 degrees W).
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