Highly silicifed, thinly bedded rocks in the immediate footwall of the No. 5 zone (Photo 2). In a TiO2-Zr plot, these rocks plot in the field of altered sediments, which lies at much lower TiO2 contents than the mafic volcanic rock trend shown in Photo 6 (Macdonald et al. 1996).





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.