Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Economic Geology Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Economic Geology; November 1966; v. 61; no. 7; p. 1291-1292
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 Hagner, A. F.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The Precambrian magnetite deposits of New York and New Jersey

A. F. Hagner

A number of lines of evidence support the view that the gneissic host rock of the iron deposits is a product of granitization and that the iron deposits were formed by release of iron from ferromagnesian silicates during regional metamorphism. (See Buddington, ibid., v. 61, p. 484-510).

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