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|Title:||Applications of mössbauer spectroscopy in meteoritical and planetary science, part i: Undifferentiated meteorites|
|Authors:||Maksimova, A. A.|
Oshtrakh, M. I.
|Citation:||Maksimova A. A. Applications of mössbauer spectroscopy in meteoritical and planetary science, part i: Undifferentiated meteorites / A. A. Maksimova, M. I. Oshtrakh. — DOI 10.3390/min11060614 // Minerals. — 2021. — Vol. 11. — Iss. 6. — 614.|
|Abstract:||Mössbauer (nuclear γ-resonance) spectroscopy is a powerful technique that is actively used in various fields, from physics and chemistry to biology and medicine. Rudolf L. Mössbauer, who observed nuclear γ-resonance and published his results in 1958, received a Nobel Prize in physics in 1961 for this discovery. The57 Fe is the most widely used nucleus in Mössbauer spectroscopy. Therefore, a large variety of compounds containing iron can be studied by Mössbauer spectroscopy. It is well known that planetary matter contains various iron-bearing phases and minerals. Therefore, the extraterrestrial material from different meteorites, asteroids, and planets can be studied using 57 Fe Mössbauer spectroscopy as additional powerful technique. Two parts of this review consider the results of more than 50 years of experience of Mössbauer spectroscopy applied for the studies of various meteorites, soils, and rocks from the Moon and recent investigation of the Mars surface using two rovers equipped with miniaturized Mössbauer spectrometers. Part I will discuss known results on Mössbauer spectroscopy of undifferentiated meteorites, which are the most primitive and formed with the solar system. © 2021 by the authors. Licensee MDPI, Basel, Switzerland.|
|Keywords:||57 FE HYPERFINE INTERACTIONS|
57FE MÖSSBAUER SPECTROSCOPY
CLASSIFICATION OF H, L, AND LL ORDINARY CHONDRITES
FE2+ PARTITIONING IN SILICATE PHASES
IRON-BEARING PHASE COMPOSITION
TEMPERATURE OF CATION EQUILIBRIUM DISTRIBUTION IN SILICATE PHASES
|metadata.dc.description.sponsorship:||This work was supported by the Ministry of Science and Higher Education of the Russian Federation, project № FEUZ‐2020‐0060. The Zavaritsky Institute of Geology and Geochemistry of the Ural Branch of the Russian Academy of Sciences is supported by the Ministry of Science and Higher Education of the Russian Federation, project № AAAA‐A19‐119071090011‐6 (A.A.M.).|
|Appears in Collections:||Научные публикации, проиндексированные в SCOPUS и WoS CC|
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