Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Economic Geology Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Economic Geology; October 1970; v. 65; no. 6; p. 706-713
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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Mookherjee, A.
Right arrow Articles by Dutta, N. K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Evidence of incipient melting of sulfides along a dike contact, Geco Mine, Manitouwadge, Ontario

Asoke Mookherjee, and N. K. Dutta

Pyrrhotite-sphalerite-chalcopyrite veins in post-ore olivine diabase, contrasting textures with liquid of Fe, Zn, and Cu sulfides above incongruent melting point of pyrite with subsequent monotectic crystallization under invariant condition, phase relations in Du-Fe-Zn-S system

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
 Can MineralHome page
B. R. Frost, J. A. Mavrogenes, and A. G. Tomkins
PARTIAL MELTING OF SULFIDE ORE DEPOSITS DURING MEDIUM- AND HIGH-GRADE METAMORPHISM
Can Mineral, February 1, 2002; 40(1): 1 - 18.
[Abstract] [Full Text] [PDF]


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