Figure 14. Alteration effects at the Fetais deposit:
calculated mass changes in Fe (in wt %). Major zones of Fe addition
occur within the rhyolite A footwall to the main orebody, and also
downdip of this, in the area of an inferred synvolcanic fault that
may have bounded a sulfide depositional graben. Holes FS-13 and LC-3
have not been sampled.
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.