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 1965; v. 60; no. 7; p. 1404-1410
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 Roy, M. M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Studies on coal maceral; IV, Chlorination of exinite and fusinite

M. M. Roy

Products of chlorination suggest "that in exinite a greater proportion of disordered structure is present, and the number of condensed aromatic rings is not more than two; sulfur is more firmly bound; the number of peripheral groups is greater. Fusinites have more condensed structures, the number of hydroaromatic structures is negligible, and the number of condensed rings present is more thantwo."

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