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; April 1989; v. 84; no. 2; p. 451-452; DOI: 10.2113/gsecongeo.84.2.451
This Article
Right arrow Full Text (PDF)
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Goodfellow, W. D.
Right arrow Articles by Turner, R. J. W.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Sulfur isotope variability in sediment-hosted massive sulfide deposits as determined using the ion microprobe SHRIMP; I, An example from the Rammelsberg orebody; discussion

Wayne D. Goodfellow, and Robert J. W. Turner

Geol. Surv. Can., Ottawa, ON, Canada

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
Economic GeologyHome page
G. D. Bradshaw, S. M. Rowins, J. M. Peter, and B. E. Taylor
Genesis of the Wolverine Volcanic Sediment-Hosted Massive Sulfide Deposit, Finlayson Lake District, Yukon, Canada: Mineralogical, Mineral Chemical, Fluid Inclusion, and Sulfur Isotope Evidence
Economic Geology, January 1, 2008; 103(1): 35 - 60.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Society of Economic Geologists