| Abstract: | Resolution of the iron sites in the Mo??ssbauer spectra of Ca-Fe pyroxenoids is only partial, two doublets being apparent in each case, whereas there are up to nine cation sites in each structure. Thus the inner and outer doublets represent, respectively: two sites and two sites in Ca0.5Fe0.5SiO3 (ferrobustamite); five sites and two sites in Ca0.15Fe0.85SiO3 (pyroxferroite); and five sites and four sites in FeSiO3 (ferrosolite III). Disorder of iron and calcium which exists in the two calcium-bearing pyroxenoids is not readily apparent in the spectra. ?? 1974 Springer-Verlag. |
| Genre: | Article |
| ProdID: | 70001309 |
| Citation Author: | Dowty, E.; Lindsley, D. H. |
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| Citation End Page: | 232 |
| Citation Issue: | 3 |
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| Citation Language: | English |
| Citation Larger Work Title: | Contributions to Mineralogy and Petrology |
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| Citation Publisher: | Springer-Verlag |
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| Citation Search Results Text: | Mo??ssbauer spectra of synthetic Ca-Fe pyroxenoids and lunar pyroxferroite; 1974; Article; Journal; Contributions to Mineralogy and Petrology; Dowty, E.; Lindsley, D. H. |
| Citation Start Page: | 229 |
| Citation Volume: | 48 |
| Citation Year: | 1974 |
| Type: | citation/reference |
| Text: | Mo??ssbauer spectra of synthetic Ca-Fe pyroxenoids and lunar pyroxferroite; 1974; Article; Journal; Contributions to Mineralogy and Petrology; Dowty, E.; Lindsley, D. H. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1007/BF00383358 |
| Date Other: | Tue, 28 Sep 2010 23:09 -0500 |
| Publisher: | Springer-Verlag |
