Continuous intersection of massive and semi-massive sulfides at Hidden Creek, located within silicified to biotite-chlorite-altered sediments just above footwall mafic volcanic rocks. The sulfides are dominantly py-po, with disseminated cp, in a quartz-calcite-rich matrix.

Home - Company Profile - Global Portfolio - Mineral Deposit Publications
Methodology - General Research Publications - Contact Us

Page design copyright © 1998 Palomar Media Corporation. All rights reserved.
Registered trademarks are used under license and are the property of their respective owners.