Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Economic Geology Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Economic Geology; November 1966; v. 61; no. 7; p. 1191-1204
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 Brown, J. S.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Ore lead isotopes of the British Isles and Scandinavia

John S. Brown

It is concluded that British leads typify generation from normal marine sediments to which they correspond broadly in age. Deposition probably was due to igneous influence in some cases and not in others, and metamorphism is lacking. Norwegian leads are similar, but mild contamination, presumably from the Precambrian, was added by Caledonian metamorphism. Swedish Phanerozoic leads are highly contaminated by radiogenic lead selectively extracted from the Precambrian basement.

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