2003
DOI: 10.1111/j.1945-5100.2003.tb00290.x
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Systematics of Mössbauer absorption areas in ordinary chondrites and applications to a newly fallen meteorite in Jodhpur, India

Abstract: Abstract-Mössbauer absorption areas corresponding to 57 Fe in olivine, pyroxene, troilite, and the metallic phase in ordinary chondrites are shown to exhibit certain systematic behaviors. H chondrites occupy 2 distinct regions on the plot of metallic phase absorption area versus silicate absorption area, while L/LL chondrites fall in a separate region. Similar separation is also observed when pyroxene absorption area is plotted against olivine absorption area. The one-dimensional plot for the ratio of olivine … Show more

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Cited by 55 publications
(75 citation statements)
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“…Similar values were taken from the literature for 3 following meteorites: Bandog [4], Bhawad [4], Tuxtuac [4]. The range of these values are shown in Table 4.…”
Section: Metallic Phasesupporting
confidence: 55%
See 1 more Smart Citation
“…Similar values were taken from the literature for 3 following meteorites: Bandog [4], Bhawad [4], Tuxtuac [4]. The range of these values are shown in Table 4.…”
Section: Metallic Phasesupporting
confidence: 55%
“…In early 2000 a Mössbauer group from India started systematic studies on the possibility of the application of Mössbauer spectroscopy to the classification of ordinary chondrites [2][3][4]. Using different types of plots such as "areas for metallic phases vs. areas for nonmetallic phases", "areas for metallic phases vs. areas for silicate phases" and "areas for pyroxene vs. areas for olivine" this group determined regions for H, L and LL types of the meteorites.…”
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. 7).…”
Section: Cosmochemical Applicationmentioning
confidence: 99%
“…For this purpose the new classification of meteorites, suggested by Verma et al [5] and based on Mössbauer spectroscopy, was applied.…”
Section: Introductionmentioning
confidence: 99%
“…Mössbauer spectroscopy was often used to investigate various types of meteorites [1][2][3][4][5][6].…”
Section: Introductionmentioning
confidence: 99%