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; July 1960; v. 55; no. 4; p. 844-847
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 Markham, N. L.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The willemite-hemimorphite relationship

N. L. Markham

Discusses factors accounting for the preferential development of willemite (rather than hemimorphite) in the oxidized zone of certain sphalerite-bearing ore deposits in South-West Africa in the light of recently published investigations of the stability of minerals in the ZnO-SiO 2 - H 2 O system.

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
 Economic GeologyHome page
M. W. Hitzman, M. W. Hitzman, N. A. Reynolds, D. F. Sangster, C. R. Allen, and C. E. Carman
Classification, Genesis, and Exploration Guides for Nonsulfide Zinc Deposits
Economic Geology, June 1, 2003; 98(4): 685 - 714.
[Abstract] [Full Text] [PDF]


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