Goldman, Don S. and Rossman, George R. (1982) The identification of Fe^(2+) in the M4 site of calcic amphiboles: reply. American Mineralogist, 67 (3-4). pp. 340-342. ISSN 0003-004X. https://resolver.caltech.edu/CaltechAUTHORS:20130510-104510612
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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.
| Item Type: | Article | ||||||
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| Additional Information: | © 1982 Mineralogical Society of America. Manuscript received, July 30, 1981; accepted for publication, October 28, 1981. | ||||||
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| Issue or Number: | 3-4 | ||||||
| Record Number: | CaltechAUTHORS:20130510-104510612 | ||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20130510-104510612 | ||||||
| Official Citation: | Goldman, Don S. and Rossman, George R. (1982) The identification of Fe^(2+) in the M4 site of calcic amphiboles: reply. American Mineralogist, 67 (3-4). pp. 340-342. ISSN 0003-004X | ||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | ||||||
| ID Code: | 38419 | ||||||
| Collection: | CaltechAUTHORS | ||||||
| Deposited By: | Tony Diaz | ||||||
| Deposited On: | 13 May 2013 19:05 | ||||||
| Last Modified: | 26 Nov 2019 11:15 |
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