Landing/Twin Creeks

The Landing Zone and Twin Creeks zones hosts gold mineralization in quartz and quartz-carbonate veins, breccia zones and stockworks often with 2 to 5% fine disseminated pyrite and occasional visible gold. Mineralization is often associated with deformed syenitic dykes within a wide deformation zone of highly altered ultramafic and mafic volcanics. Mafic volcanics show pervasive carbonate (ankerite) and sericite alteration with varying silicification. Potential for a significant underground and high grade deposit remains below currently tested depths.
Copyright © 2019 by Moneta Porcupine Mines Inc.   All rights reserved worldwide.
For more information, send questions and comments to
This page was created on Sat Feb 16, 2019 at 3:47:42 AM Pacific Time.