Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist RIMG advertisement
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; April 1983; v. 68; no. 3-4; p. 456-458
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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Deliens, M.
Right arrow Articles by Piret, P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Metastudtite, UO 4 . 2H 2 O, a new mineral from Shinkolobwe, Shaba, Zaire

Michel Deliens, and Paul Piret

Mus. R. Afr. Cent., Dep. Geol., Tervuren, Belgium
Univ. Louvain, Belgium

Aggregates of flexible pale yellow fibers. Electron microprobe analysis gave UO 4 88.1%. H 2 O by TGA approximately 10%. Powder data similar to heated studtite (UO 4 . 4H 2 O). Orthorhombic, probable space group Immm, a = 6.51(1), b = 8.78(2), c = 4.21(1)Aa, Z = 2, d(calc.) = 4.67 mg/cm 3 . Strongest lines in the X-ray powder pattern are 5.22 (100)(110), 3.54 (80) (101), 4.38 (50)(020) and 3.79 (50)(011). Optically biaxial positive. gamma = 1.760 (parallel to c, fiber axis), beta = 1.658 and alpha = 1.640.--Modified journal abstract.

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
Geological Society, London, Special PublicationsHome page
E. C. Buck, B. D. Hanson, and B. K. McNamara
The geochemical behaviour of Tc, Np and Pu in spent nuclear fuel in an oxidizing environment
Geological Society, London, Special Publications, January 1, 2004; 236(1): 65 - 88.
[Abstract] [PDF]


Home page
American MineralogistHome page
P. C. Burns and K.-A. Hughes
Studtite, [(UO2)(O2)(H2O)2](H2O)2: The first structure of a peroxide mineral
American Mineralogist, July 1, 2003; 88(7): 1165 - 1168.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2010 by Mineralogical Society of America