Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Economic Geology GSW 2008 Users' Group Meeting
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Economic Geology; August 1968; v. 63; no. 5; p. 573-574
This Article
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Right arrow Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Joralemon, P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The Wilbur Springs quicksilver district

Peter Joralemon

Certain ore bodies have been worked for gold as well as quicksilver. The gold-mercury ratio increases toward the center of the district and downward, suggesting zoning about a high-intensity core and a common origin for both metals. Since gold is deficient in surrounding sediments, of the two possible sources for the ore fluid suggested by Moiseyev, the magmatic seems the more likely. (Original paper, ibid., v. 63, p. 169-181, 1968.)

This record provided courtesy of AGI/GeoRef.






JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Society of Economic Geologists