Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
European Journal of Mineralogy Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

European Journal of Mineralogy; April 2003; v. 15; no. 2; p. 427-433; DOI: 10.1127/0935-1221/2003/0015-0427
© 2003 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
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 Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by CABELLA, R.
Right arrow Articles by NAYAK, V. K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Articles

Squawcreekite-rutile solid solution from the Kajlidongri Mine (India)

Roberto CABELLA1,*, Riccardo BASSO1, Gabriella LUCCHETTI1, Pietro MARESCOTTI1, Alberto MARTINELLI1 and Virendra Kumar NAYAK2

1 Dipartimento per lo Studio del Territorio e delle sue Risorse, Università di Genova, Corso Europa 26, I-16132 Genova, Italy
2 Department of Applied Geology, University of Saugar, P.O. Saugar-3 (M.P.), India

* Corresponding author, e-mail: cabella{at}dipteris.unige.it

Squawcreekite is a rare AO2 oxide with rutile-type structure. A squawcreekite (FeSbO4)-rutile (TiO2) solid solution has been recognised in quartz veins from the Kajlidongri manganese mine District Jhabua, Madhya Pradesh (India): this finding represents the first occurrence of a chemically pure squawcreekite-rutile solid solution. Transmission electron microscopy analyses exclude the existence of intergrowths or microinclusions, as well as spinodal decomposition. Quantitative electron microprobe analyses clearly indicate that the exchange vector Fe3+Sb5+Ti4+-2 accounts for the wide compositional variation suggesting the existence of a solubility range in natural samples between rutile70squawcreekite30 — rutile30squawcreekite70.

Key-words: squawcreekite, rutile, solid solution, mineral data, TEM, India..







JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers