Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
The Canadian Mineralogist Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

The Canadian Mineralogist; August 2001; v. 39; no. 4; p. 1065-1071; DOI: 10.2113/gscanmin.39.4.1065
© 2001 Mineralogical Association of Canada
This Article
Right arrow Résumé
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
Right arrow Citation Map
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Grice, J. D.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Articles

THE CRYSTAL STRUCTURE OF FENCOOPERITE: UNIQUE [Fe3+3O13] PINWHEELS CROSS-CONNECTED BY [Si8O22] ISLANDS

Joel D. Grice§

Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada

§ E-mail address: jgrice{at}mus-nature.ca

The crystal structure of fencooperite, ideally Ba6Fe3+3Si8O23(CO3)2Cl3·H2O, has been solved in the trigonal space-group P3m1, with a 10.7409(5), c 7.0955(4) Å, V 708.9(1) Å3 and Z = 1. The final residual index for observed reflections is 0.038. The uniqueness of the fencooperite structure is a result of two previously unknown fundamental building blocks (FBB). The islands of silica tetrahedra form [Si8O22] units described as double open-branched triple tetrahedra sharing vertices along [001]. The other unique FBB consists of three (Fe3+O5) tetragonal pyramids having one of the O atoms common to all three polyhedra, forming a pinwheel trimer [Fe3O13]. The pronounced optical absorption is attributed to this coordination complex of iron. This trimer cross-links the [Si8O22] islands to form a framework structure. The framework supports intersecting tunnels in all three crystallographic directions that are filled by Ba and Cl atoms and by H2O and CO3 groups. The structure of fencooperite is compared to that of gillespite, pellyite, titantaramellite and orthoericssonite. In gillespite and pellyite, individual polyhedra of Fe2+ in four-fold coordination with oxygen cross-link sheets and chains of silica tetrahedra, whereas the chains of Fe3+ in (titan)taramellite having six-fold coordination with oxygen cross-links island rings of silica tetrahedra. In orthoericssonite, which has the same five-fold coordination of Fe3+ as fencooperite, the Fe3+ polyhedra cross-link [Si2O7] groups into sheets.

Keywords: fencooperite, unique crystal structure, hydrated barium–iron silicate–carbonate–chloride, ferric iron, five-fold coordination, pinwheel.




This article has been cited by other articles:


Home page
Can MineralHome page
L. C. Basciano and L. A. Groat
THE CRYSTAL STRUCTURE OF KAMPFITE
Can Mineral, August 1, 2007; 45(4): 935 - 943.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
J. D. Grice
THE STRUCTURE OF SPURRITE, TILLEYITE AND SCAWTITE, AND RELATIONSHIPS TO OTHER SILICATE CARBONATE MINERALS
Can Mineral, October 1, 2005; 43(5): 1489 - 1500.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
L. C. Basciano, L. A. Groat, A. C. Roberts, J. D. Grice, G. E. Dunning, E. E. Foord, I. M. Kjarsgaard, and R. E. Walstrom
KAMPFITE, A NEW BARIUM SILICATE CARBONATE MINERAL SPECIES FROM FRESNO COUNTY, CALIFORNIA
Can Mineral, August 1, 2001; 39(4): 1053 - 1058.
[Abstract] [Full Text] [PDF]




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