Published March 1982
| public
Journal Article
The identification of Fe^(2+) in the M4 site of calcic amphiboles: reply
- Creators
- Goldman, Don S.
-
Rossman, George R.
Chicago
An error occurred while generating the citation.
Abstract
Experimental evidence indicates that absorption from Fe^(2+) in the M4 site dominates the optical spectrum of most calcic amphiboles in the 1000 nm region in the spectrum. Contributions from Fe^(2+) in M1, M2 and M3 occur in the 850-1150 nm region, but the intrinsic intensity of absorption by Fe^(2+) in these sites is much less than that of Fe^(2+) in M4.
Additional Information
© 1982 Mineralogical Society of America. Manuscript received, July 30, 1981; accepted for publication, October 28, 1981.Additional details
- Eprint ID
- 38419
- Resolver ID
- CaltechAUTHORS:20130510-104510612
- Created
-
2013-05-13Created from EPrint's datestamp field
- Updated
-
2019-11-26Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)
- Other Numbering System Name
- Caltech Division of Geological and Planetary Sciences
- Other Numbering System Identifier
- 3661