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Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy

Bibliographic Details
Main Author: Maksimova, A A.
Publication Date: 2020
Other Authors: Petrova, E. V., Chukin, A. V., Karabanalov, M. S., Nogueira, Bernardo Albuquerque, Fausto, Rui, Yesiltas, M., Felner, I., Oshtrakh, M. I.
Format: Article
Language: eng
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: https://hdl.handle.net/10316/99964
https://doi.org/10.1016/j.saa.2020.118723
Summary: The bulk interior of Kemer L4 ordinary chondrite was characterized for the first time bymeans of opticalmicroscopy, scanning electronmicroscopywith energy dispersive spectroscopy, Raman spectroscopy, X-ray diffraction, magnetizationmeasurements andMössbauer spectroscopy with a high velocity resolution. The main andminor iron-bearing phaseswere found aswell as ferrihydrite as a result ofweathering. The Fe2+ partitioning among the M1andM2 sites in olivine, orthopyroxene and clinopyroxenewas determined fromthe 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 Xray 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.
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spelling Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopyKemer L4 ordinary chondriteX-ray diffractionRaman spectroscopyMagnetization measurementsMössbauer spectroscopyThe bulk interior of Kemer L4 ordinary chondrite was characterized for the first time bymeans of opticalmicroscopy, scanning electronmicroscopywith energy dispersive spectroscopy, Raman spectroscopy, X-ray diffraction, magnetizationmeasurements andMössbauer spectroscopy with a high velocity resolution. The main andminor iron-bearing phaseswere found aswell as ferrihydrite as a result ofweathering. The Fe2+ partitioning among the M1andM2 sites in olivine, orthopyroxene and clinopyroxenewas determined fromthe 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 Xray 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.Elsevier2020-07-20info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttps://hdl.handle.net/10316/99964https://hdl.handle.net/10316/99964https://doi.org/10.1016/j.saa.2020.118723eng1386-1425Maksimova, A A.Petrova, E. V.Chukin, A. V.Karabanalov, M. S.Nogueira, Bernardo AlbuquerqueFausto, RuiYesiltas, M.Felner, I.Oshtrakh, M. I.info:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2022-09-01T13:17:13Zoai:estudogeral.uc.pt:10316/99964Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-29T05:48:53.552359Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
title Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
spellingShingle Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
Maksimova, A A.
Kemer L4 ordinary chondrite
X-ray diffraction
Raman spectroscopy
Magnetization measurements
Mössbauer spectroscopy
title_short Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
title_full Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
title_fullStr Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
title_full_unstemmed Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
title_sort Characterization of Kemer L4meteorite using Raman spectroscopy, X-ray diffraction, magnetization measurements and Mössbauer spectroscopy
author Maksimova, A A.
author_facet Maksimova, A A.
Petrova, E. V.
Chukin, A. V.
Karabanalov, M. S.
Nogueira, Bernardo Albuquerque
Fausto, Rui
Yesiltas, M.
Felner, I.
Oshtrakh, M. I.
author_role author
author2 Petrova, E. V.
Chukin, A. V.
Karabanalov, M. S.
Nogueira, Bernardo Albuquerque
Fausto, Rui
Yesiltas, M.
Felner, I.
Oshtrakh, M. I.
author2_role author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Maksimova, A A.
Petrova, E. V.
Chukin, A. V.
Karabanalov, M. S.
Nogueira, Bernardo Albuquerque
Fausto, Rui
Yesiltas, M.
Felner, I.
Oshtrakh, M. I.
dc.subject.por.fl_str_mv Kemer L4 ordinary chondrite
X-ray diffraction
Raman spectroscopy
Magnetization measurements
Mössbauer spectroscopy
topic Kemer L4 ordinary chondrite
X-ray diffraction
Raman spectroscopy
Magnetization measurements
Mössbauer spectroscopy
description The bulk interior of Kemer L4 ordinary chondrite was characterized for the first time bymeans of opticalmicroscopy, scanning electronmicroscopywith energy dispersive spectroscopy, Raman spectroscopy, X-ray diffraction, magnetizationmeasurements andMössbauer spectroscopy with a high velocity resolution. The main andminor iron-bearing phaseswere found aswell as ferrihydrite as a result ofweathering. The Fe2+ partitioning among the M1andM2 sites in olivine, orthopyroxene and clinopyroxenewas determined fromthe 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 Xray 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.
publishDate 2020
dc.date.none.fl_str_mv 2020-07-20
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://hdl.handle.net/10316/99964
https://hdl.handle.net/10316/99964
https://doi.org/10.1016/j.saa.2020.118723
url https://hdl.handle.net/10316/99964
https://doi.org/10.1016/j.saa.2020.118723
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 1386-1425
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologia
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instname_str FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologia
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institution RCAAP
reponame_str Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
collection Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
repository.name.fl_str_mv Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologia
repository.mail.fl_str_mv info@rcaap.pt
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