Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
American Mineralogist Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
American Mineralogist; February 1983; v. 68; no. 1-2; p. 255-261
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 Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Giese, R. F.
Right arrow Articles by Penna, G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The crystal structure of sulfoborite, Mg 3 SO 4 (B(OH) 4 ) 2 (OH)F

R. F. Giese, and G. Penna

Roswell Park Mem. Inst., Cent. Crystallogr. Res., Buffalo, NY, United States
Hooker Chem. Corp., United States

Orthorhombic, space group Pnma with a = 10.132, b = 12.537 and c = 7.775Aa (all + or -0.001Aa). There are four formula units in the unit cell. The two types of octahedra share an edge and/or corners among themselves. The sulfate tetrahedron shares corners with both types of octahedra and these three units form crude sheets centered about the mirror planes. The sheets are jointed by the boron tetrahedra into a three-dimensional structure.--Modified journal abstract.

This record provided courtesy of AGI/GeoRef.






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