2016
DOI: 10.1007/s10751-016-1215-7
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Comparative study of Aliskerovo, Anyujskij, Sikhote-Alin and Sterlitamak iron meteorites using Mössbauer spectroscopy

Abstract: A comparative study of Sikhote-Alin IIAB, Anyujskij IIAB, Aliskerovo IIIE-an and Sterlitamak IIIAB iron meteorites was carried out using Mössbauer spectroscopy with a high velocity resolution as well as using metallography, scanning electron microscopy with energy dispersive spectroscopy and X-ray diffraction. Different numbers of spectral components were found in the Mössbauer spectra of Sikhote-Alin IIAB and Anyujskij IIAB and in the spectra of Aliskerovo IIIE-an and Sterlitamak IIIAB iron meteorites. The va… Show more

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Cited by 7 publications
(10 citation statements)
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“…The magnetic sextets 1 and 3 were assigned to the octahedral [B] and tetrahedral (A) sites in γ-Fe2O3, respectively (δ = 0.397 mm/s, Heff = 501.1 kOe, A = ~4.8% and δ = 0.277 mm/s, Heff = 483.9 kOe, A = ~10.3%), sextets 2, 4, and 5 were related to the (A), [B1], and [B2] sites in Fe3O4, respectively (δ = 0.332 mm/s, Heff = 494.0 kOe, A = ~13.3%; δ = 0.425 mm/s, Heff = 472.8 kOe, A = ~4.2% and δ = 0.578 mm/s, Heff = 449.0 kOe, A = ~8.5%), sextets 6, 7, and 8 were associated with α-FeOOH magnetic particles with different sizes, respectively (δ = 0.380 mm/s, Heff = 326.4 kOe, A = ~8.5%; δ = 0.316 mm/s, Heff = 253.9 kOe, A = ~9.8% and δ = 0.286 mm/s, Heff = 189.6 kOe, A = ~8.2%), and quadrupole doublets 9, 10, and 11 were assigned to the paramagnetic FeOOH particles, respectively (δ = 0.444 mm/s, ΔEQ = 1.033 mm/s, A = ~15.8%; δ = 0.389 mm/s, ΔEQ = 0.782 mm/s, A = ~2.6%, and δ = 0.390 mm/s, ΔEQ = 0.503 mm/s, A = ~14.1%). The fit of these and other spectra measured with a high velocity resolution in [81][82][83][84] revealed more spectral components compared to that in the low velocity resolution spectra measured in [75]. Synchrotron Mössbauer spectroscopy was applied to study the Tazewell IAB-sLH iron meteorite with a spatial resolution of ~10-20 μm in [43,44].…”
Section: Iron Meteoritesmentioning
confidence: 99%
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“…The magnetic sextets 1 and 3 were assigned to the octahedral [B] and tetrahedral (A) sites in γ-Fe2O3, respectively (δ = 0.397 mm/s, Heff = 501.1 kOe, A = ~4.8% and δ = 0.277 mm/s, Heff = 483.9 kOe, A = ~10.3%), sextets 2, 4, and 5 were related to the (A), [B1], and [B2] sites in Fe3O4, respectively (δ = 0.332 mm/s, Heff = 494.0 kOe, A = ~13.3%; δ = 0.425 mm/s, Heff = 472.8 kOe, A = ~4.2% and δ = 0.578 mm/s, Heff = 449.0 kOe, A = ~8.5%), sextets 6, 7, and 8 were associated with α-FeOOH magnetic particles with different sizes, respectively (δ = 0.380 mm/s, Heff = 326.4 kOe, A = ~8.5%; δ = 0.316 mm/s, Heff = 253.9 kOe, A = ~9.8% and δ = 0.286 mm/s, Heff = 189.6 kOe, A = ~8.2%), and quadrupole doublets 9, 10, and 11 were assigned to the paramagnetic FeOOH particles, respectively (δ = 0.444 mm/s, ΔEQ = 1.033 mm/s, A = ~15.8%; δ = 0.389 mm/s, ΔEQ = 0.782 mm/s, A = ~2.6%, and δ = 0.390 mm/s, ΔEQ = 0.503 mm/s, A = ~14.1%). The fit of these and other spectra measured with a high velocity resolution in [81][82][83][84] revealed more spectral components compared to that in the low velocity resolution spectra measured in [75]. Synchrotron Mössbauer spectroscopy was applied to study the Tazewell IAB-sLH iron meteorite with a spatial resolution of ~10-20 μm in [43,44].…”
Section: Iron Meteoritesmentioning
confidence: 99%
“…A comparative study of iron meteorites Anyujskij IIAB, Sikhote-Alin IIAB, Aliskerovo IIIE-an, and Sterlitamak IIIAB was carried out using Mössbauer spectroscopy with a high velocity resolution in [81,82] The comparison of powdered samples of one fragment of Chinga iron-ung, in which visually different areas (1, 2, 3, 4, and 5) of the saw-cut surface were observed, was done using Mössbauer spectroscopy with a high velocity resolution (4096 channels) in [80]. The Mössbauer spectra of these samples obtained from four areas are shown in Figure 31.…”
Section: Iron Meteoritesmentioning
confidence: 99%
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