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A high spatial resolution synchrotron Mössbauer study of the Tazewell IIICD and Esquel pallasite meteorites
Author(s) -
Blukis Roberts,
Rüffer Rudolf,
Chumakov Aleksandr I.,
Harrison Richard J.
Publication year - 2017
Publication title -
meteoritics and planetary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.09
H-Index - 100
eISSN - 1945-5100
pISSN - 1086-9379
DOI - 10.1111/maps.12841
Subject(s) - kamacite , meteorite , mössbauer spectroscopy , synchrotron , troilite , spectral line , phase (matter) , spectroscopy , geology , transect , hyperfine structure , paramagnetism , materials science , mineralogy , chemistry , analytical chemistry (journal) , nuclear magnetic resonance , crystallography , physics , optics , chondrite , condensed matter physics , atomic physics , astrobiology , oceanography , organic chemistry , astronomy , chromatography , quantum mechanics
Metallic phases in the Tazewell IIICD iron and Esquel pallasite meteorites were examined using 57 Fe synchrotron Mössbauer spectroscopy. Spatial resolution of ~10–20 μm was achieved, together with high throughput, enabling individual spectra to be recorded in less than 1 h. Spectra were recorded every 5–10 μm, allowing phase fractions and hyperfine parameters to be traced along transects of key microstructural features. The main focus of the study was the transitional region between kamacite and plessite, known as the “cloudy zone.” Results confirm the presence of tetrataenite and antitaenite in the cloudy zone as its only components. However, both phases were also found in plessite, indicating that antitaenite is not restricted exclusively to the cloudy zone, as previously thought. The confirmation of paramagnetic antitaenite as the matrix phase of the cloudy zone contrasts with recent observations of a ferromagnetic matrix phase using X‐ray photoemission electron spectroscopy. Possible explanations for the different results seen using these techniques are proposed.