Mössbauer spectroscopic study on the composition of Fe-containing minerals in ordinary chondrites, Miller Range 07710 and Yamato 790272

W. Sato; M. Nakagawa; N. Shirai; M. Ebihara

doi:10.1007/s10751-018-1489-z

Mössbauer spectroscopic study on the composition of Fe-containing minerals in ordinary chondrites, Miller Range 07710 and Yamato 790272

W. Sato^*, M. Nakagawa, N. Shirai, M. Ebihara

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

6 Citations (Scopus)

Abstract

⁵⁷Fe Mössbauer spectroscopy was applied to compositional studies of Fe-containing minerals in two different ordinary chondrites, MIL 07710 (L4) and Y-790272 (H4), collected in Antarctica. For both samples, spectral analysis revealed that there are five quadrupole doublets and two magnetic sextets in the room-temperature spectra, suggesting the presence of olivine (M1 and M2), pyroxene (M1 and M2), a high-spin Fe³⁺ containing phase, antiferromagnetic FeS (troilite), and ferromagnetic Fe-Ni alloy. The large relative area of the oxidized Fe³⁺ phases and the small intensity of the metal phases signify a possible effect of terrestrial weathering especially for Y-790272 (H4).

Original language	English
Article number	13
Journal	Hyperfine Interactions
Volume	239
Issue number	1
DOIs	https://doi.org/10.1007/s10751-018-1489-z
Publication status	Published - 2018 Dec 1
Externally published	Yes

Keywords

Chondrite
MIL 07710
Meteorite
Mössbauer spectroscopy
Terrestrial weathering
Y-790272

ASJC Scopus subject areas

Atomic and Molecular Physics, and Optics
Nuclear and High Energy Physics
Condensed Matter Physics
Physical and Theoretical Chemistry

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10.1007/s10751-018-1489-z

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title = "M{\"o}ssbauer spectroscopic study on the composition of Fe-containing minerals in ordinary chondrites, Miller Range 07710 and Yamato 790272",

abstract = "57Fe M{\"o}ssbauer spectroscopy was applied to compositional studies of Fe-containing minerals in two different ordinary chondrites, MIL 07710 (L4) and Y-790272 (H4), collected in Antarctica. For both samples, spectral analysis revealed that there are five quadrupole doublets and two magnetic sextets in the room-temperature spectra, suggesting the presence of olivine (M1 and M2), pyroxene (M1 and M2), a high-spin Fe3+ containing phase, antiferromagnetic FeS (troilite), and ferromagnetic Fe-Ni alloy. The large relative area of the oxidized Fe3+ phases and the small intensity of the metal phases signify a possible effect of terrestrial weathering especially for Y-790272 (H4).",

keywords = "Chondrite, MIL 07710, Meteorite, M{\"o}ssbauer spectroscopy, Terrestrial weathering, Y-790272",

author = "W. Sato and M. Nakagawa and N. Shirai and M. Ebihara",

note = "Funding Information: The present work was supported in part by JSPS KAKENHI Grant Number 26286075. Publisher Copyright: {\textcopyright} 2018, Springer International Publishing AG, part of Springer Nature.",

year = "2018",

month = dec,

day = "1",

doi = "10.1007/s10751-018-1489-z",

language = "English",

volume = "239",

journal = "Hyperfine Interaction",

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T1 - Mössbauer spectroscopic study on the composition of Fe-containing minerals in ordinary chondrites, Miller Range 07710 and Yamato 790272

AU - Sato, W.

AU - Nakagawa, M.

AU - Shirai, N.

AU - Ebihara, M.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - 57Fe Mössbauer spectroscopy was applied to compositional studies of Fe-containing minerals in two different ordinary chondrites, MIL 07710 (L4) and Y-790272 (H4), collected in Antarctica. For both samples, spectral analysis revealed that there are five quadrupole doublets and two magnetic sextets in the room-temperature spectra, suggesting the presence of olivine (M1 and M2), pyroxene (M1 and M2), a high-spin Fe3+ containing phase, antiferromagnetic FeS (troilite), and ferromagnetic Fe-Ni alloy. The large relative area of the oxidized Fe3+ phases and the small intensity of the metal phases signify a possible effect of terrestrial weathering especially for Y-790272 (H4).

AB - 57Fe Mössbauer spectroscopy was applied to compositional studies of Fe-containing minerals in two different ordinary chondrites, MIL 07710 (L4) and Y-790272 (H4), collected in Antarctica. For both samples, spectral analysis revealed that there are five quadrupole doublets and two magnetic sextets in the room-temperature spectra, suggesting the presence of olivine (M1 and M2), pyroxene (M1 and M2), a high-spin Fe3+ containing phase, antiferromagnetic FeS (troilite), and ferromagnetic Fe-Ni alloy. The large relative area of the oxidized Fe3+ phases and the small intensity of the metal phases signify a possible effect of terrestrial weathering especially for Y-790272 (H4).

KW - Chondrite

KW - MIL 07710

KW - Meteorite

KW - Mössbauer spectroscopy

KW - Terrestrial weathering

KW - Y-790272

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JO - Hyperfine Interaction

JF - Hyperfine Interaction

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Mössbauer spectroscopic study on the composition of Fe-containing minerals in ordinary chondrites, Miller Range 07710 and Yamato 790272

Abstract

Keywords

ASJC Scopus subject areas

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