Cross sectional view of Jons Trend (NE side of trend, A-A’, and SE side of trend, B-B’) with recent drilling indicated. Geological model has defined tight isoclinal folding of metasedimentary units (greys) that are near upright and parallel to shearing as well as the strike of mineralization at Jons Trend (orange vein zones).
Cross sectional view of Jons Trend (NE side of trend, A-A’, and SE side of trend, B-B’) with recent drilling indicated. Geological model has defined tight isoclinal folding of metasedimentary units (greys) that are near upright and parallel to shearing as well as the strike of mineralization at Jons Trend (orange vein zones).