Vesuvianite From Pajsberg, Sweden, and the Role of Be In the Vesuvianite Structure
Abstract
Vesuvianite from Pajsberg, Sweden contains about one atom of Mn, based on 50 cations per formula unit, and small amounts of Be, B, and As. Optical absorption analysis suggests that the Mn is predominantly or entirely trivalent. Crystal-structure analysis indicates that Mn is housed at the general octahedral site Y3, which exhibits only minor distortion from ideal octahedral symmetry. Arsenic is housed at Y2 and Z2, and the formula derived from electron microprobe and LA-ICP-MS analyses suggests minor substitution of Al for Si, also at Z2. Beryllium and B are at T1, between the edge-sharing trimers Y3Y2Y3, as is the case for B in the boron-dominant vesuvianite species wiluite. The total content at T1 is interpreted as 0.82Be, 0.34B, and 0.037Fe^(3+).
Additional Information
© 2016 Mineralogical Association of Canada. Received April 23, 2015. Revised manuscript accepted May 5, 2016. Lee A. Groat and Ulf Halenius provided numerous helpful comments. Funding was provided, in part, by NSF grants EAR 89-16064 and EAR 1322082 to GRR.Attached Files
Published - 1525.full.pdf
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Additional details
- Eprint ID
- 78595
- Resolver ID
- CaltechAUTHORS:20170627-084006790
- NSF
- EAR 89-16064
- NSF
- EAR-1322082
- Created
-
2017-06-27Created from EPrint's datestamp field
- Updated
-
2021-11-15Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)