2008
DOI: 10.1111/j.1945-5100.2008.tb01091.x
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A study of ordinary chondrites by Mössbauer spectroscopy with high‐velocity resolution

Abstract: Abstract-An improvement in the velocity resolution and quality of Mössbauer spectra has been applied to a group of ordinary chondrites. This improvement permitted us to carry out a more detailed study of the iron bearing phases in these samples than has previously been possible. Mössbauer spectra of 11 ordinary chondrites of L and H chemical groups were measured using 4096 channels and presented for further analysis in 1024 channels. Subspectra of the metal grains of several chondrites demonstrated the presenc… Show more

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Cited by 63 publications
(52 citation statements)
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“…Similar values were taken from the literature for two following meteorites: Kunashak [9] and New Halfa [12]. The range of these values are shown in Table 3.…”
Section: Metallic Phasesupporting
confidence: 57%
See 1 more Smart Citation
“…Similar values were taken from the literature for two following meteorites: Kunashak [9] and New Halfa [12]. The range of these values are shown in Table 3.…”
Section: Metallic Phasesupporting
confidence: 57%
“…[8], Ochansk [9], Richardton [9], Torino [10], Vengerovo [9], Xingyang [11], Zvonkov [9]. The range of these values are shown in Table 2.…”
Section: Metallic Phasementioning
confidence: 99%
“…Ten meteorites were measured in our laboratory. Results of nine other meteorites were taken from the literature [6,[10][11][12][13].…”
Section: Methodsmentioning
confidence: 99%
“…Mössbauer spectroscopy was often used to investigate various types of meteorites [1][2][3][4][5][6].…”
Section: Introductionmentioning
confidence: 99%
“…However, investigations of some meteorites samples using Mössbauer spectroscopy with a high velocity resolution demonstrated new results in revealing of spectral components which cannot be obtained from the low velocity resolution Mössbauer spectra [12,[27][28][29][30]. For instance, in the study of ordinary chondrites it was possible to fit complicated Mössbauer spectra using components related to the crystallographically non-equivalent M1 and M2 sites occupied by both Fe 2+ and Mg 2+ ions in both pyroxene (Fe,Mg)SiO 3 and olivine (Fe,Mg) 2 SiO 4 while in the low velocity resolution spectra this was not possible (see comparison of Mössbauer spectra of ordinary chondrites measured in [31] with a low velocity resolution and with a high velocity resolution (this work) in Fig.…”
Section: Cosmochemical Applicationmentioning
confidence: 99%