Please use this identifier to cite or link to this item: http://hdl.handle.net/10316/91164
Title: Characterization of Kemer L4 meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
Authors: Maksimova, A A
Petrova, E V
Chukin, A V
Karabanalov, M S
Nogueira, Bernardo A
Rui Fausto 
Yesiltas, M
Felner, I
Oshtrakh, M I
Keywords: Kemer L4 ordinary chondrite; X-ray diffraction; Raman spectroscopy; Magnetization measurement; Mössbauer spectroscopy
Issue Date: 5-Dec-2020
Publisher: Elsevier
Project: info:eu-repo/grantAgreement/FCT/UI0313/QUI/2020/PT 
Serial title, monograph or event: Spectrochimica acta. Part A, Molecular and Biomolecular Spectroscopy
Volume: 242
Abstract: The bulk interior of Kemer L4 ordinary chondrite was characterized for the first time by means of optical microscopy, scanning electron microscopy with energy dispersive spectroscopy, Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy with a high velocity resolution. The main and minor iron-bearing phases were found as well as ferrihydrite as a result of weathering. The Fe2+ partitioning among the M1 and M2 sites in olivine, orthopyroxene and clinopyroxene was determined from the X-ray diffraction. The ratios of Fe2+ occupancies for these crystals were estimated from both X-ray diffraction and Mössbauer spectroscopy data and appeared to be in a good agreement. The distribution coefficients KD and the temperatures of equilibrium cation distribution Teq were also evaluated for olivine and orthopyroxene from two independent techniques and were in a good consistence: KD = 1.77, Teq = 441 K (X-ray diffraction) and KD = 1.77, Teq = 439 K (Mössbauer spectroscopy) for olivine and KD = 0.10, Teq = 806 K (X-ray diffraction) and KD = 0.09, Teq = 787 K (Mössbauer spectroscopy) for orthopyroxene. The fusion crust of Kemer L4 was studied using X-ray diffraction, magnetization measurements and Mössbauer spectroscopy. Magnesioferrite and probably maghemite were found in the fusion crust in addition to other phases observed in the bulk interior.
URI: http://hdl.handle.net/10316/91164
ISSN: 13861425
DOI: 10.1016/j.saa.2020.118723
Rights: embargoedAccess
Appears in Collections:I&D CQC - Artigos em Revistas Internacionais

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