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; December 1967; v. 62; no. 8; p. 1088-1091
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 Stanton, R. L.
Right arrow Articles by Rafter, T. A.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Sulfur isotope ratios in co-existing galena and sphalerite from Broken Hill, New South Wales

R. L. Stanton, and T. A. Rafter

In 15 out of 16 sphalerite-galena pairs, there has been a relative concentration of the heavier sulfur isotope in the sphalerite. Comparison of results from many areas suggests that fractionation decreases with increasing metamorphic grade. Applications to geologic thermometry may be significant.

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
 American MineralogistHome page
J. Lusk, B. O. E. Calder, and T. E. Freeman
Temperatures from triple-junction angles in sulfides
American Mineralogist, October 1, 2002; 87(10): 1390 - 1400.
[Abstract] [Full Text] [PDF]


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