Boron and chlorine abundances in Antarctic chondrites: A PGA study

P(論文) Boron and chlorine abundances were determined by prompt gamma-ray analysis for Antarctic meteorites of 22 carbonaceous chondrites and 12 ordinary chondrites. Both B and Cl contents of most Antarctic meteorites analyzed in this study are systematically higher than those for non-Antarctic chondr...

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Main Authors: Oura, Yasuji, Takahashi, Chieko, Ebihara, Mitsuru
Language:English
Published: National Institute of Polar Research 2004
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/6049/files/KJ00002352177.pdf
https://doi.org/10.15094/00006049
https://nipr.repo.nii.ac.jp/records/6049
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author Oura, Yasuji
Takahashi, Chieko
Ebihara, Mitsuru
author_facet Oura, Yasuji
Takahashi, Chieko
Ebihara, Mitsuru
author_sort Oura, Yasuji
collection National Institute of Polar Research Repository, Japan
description P(論文) Boron and chlorine abundances were determined by prompt gamma-ray analysis for Antarctic meteorites of 22 carbonaceous chondrites and 12 ordinary chondrites. Both B and Cl contents of most Antarctic meteorites analyzed in this study are systematically higher than those for non-Antarctic chondrites of corresponding groups, implying that Antarctic meteorites of carbonaceous and ordinary chondrite groups were contaminated with not only Cl (and other halogens like I) but also B. Boron and Cl contents are correlated with each other in Antarctic ordinary chondrites whereas no apparent correlation can be seen for carbonaceous chondrites. Considering that interior portions were used for carbonaceous chondrites while interior and outer portions were randomly sampled for ordinary chondrite used in this study, B and Cl are distributed differently between the two groups of chondrite, suggesting that B and Cl independently behaved following their own chemical properties after contaminant(s) carrying these elements adhered on the surface of meteorites. Sea mist is a probable candidate for such a contaminant. Leaching experiments showed that no B is essentially recovered by water and acetone even from pulverized specimens, from which a fairly large fraction of Cl is recovered, confirming that B and Cl reside independently in chondrite samples and further that both elements behaved differently after sticking to these samples on Antarctica. departmental bulletin paper
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
geographic Antarctic
geographic_facet Antarctic
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institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00006049
op_relation Antarctic meteorite research
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172
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AA11182426
https://nipr.repo.nii.ac.jp/record/6049/files/KJ00002352177.pdf
https://doi.org/10.15094/00006049
https://nipr.repo.nii.ac.jp/records/6049
publishDate 2004
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00006049 2025-04-13T14:09:27+00:00 Boron and chlorine abundances in Antarctic chondrites: A PGA study Oura, Yasuji Takahashi, Chieko Ebihara, Mitsuru 2004-09 application/pdf https://nipr.repo.nii.ac.jp/record/6049/files/KJ00002352177.pdf https://doi.org/10.15094/00006049 https://nipr.repo.nii.ac.jp/records/6049 eng eng National Institute of Polar Research Antarctic meteorite research 17 172 184 AA11182426 https://nipr.repo.nii.ac.jp/record/6049/files/KJ00002352177.pdf https://doi.org/10.15094/00006049 https://nipr.repo.nii.ac.jp/records/6049 boron chlorine Antarctic chondrite terrestrial contamination prompt 2004 ftnipr https://doi.org/10.15094/00006049 2025-03-19T10:19:56Z P(論文) Boron and chlorine abundances were determined by prompt gamma-ray analysis for Antarctic meteorites of 22 carbonaceous chondrites and 12 ordinary chondrites. Both B and Cl contents of most Antarctic meteorites analyzed in this study are systematically higher than those for non-Antarctic chondrites of corresponding groups, implying that Antarctic meteorites of carbonaceous and ordinary chondrite groups were contaminated with not only Cl (and other halogens like I) but also B. Boron and Cl contents are correlated with each other in Antarctic ordinary chondrites whereas no apparent correlation can be seen for carbonaceous chondrites. Considering that interior portions were used for carbonaceous chondrites while interior and outer portions were randomly sampled for ordinary chondrite used in this study, B and Cl are distributed differently between the two groups of chondrite, suggesting that B and Cl independently behaved following their own chemical properties after contaminant(s) carrying these elements adhered on the surface of meteorites. Sea mist is a probable candidate for such a contaminant. Leaching experiments showed that no B is essentially recovered by water and acetone even from pulverized specimens, from which a fairly large fraction of Cl is recovered, confirming that B and Cl reside independently in chondrite samples and further that both elements behaved differently after sticking to these samples on Antarctica. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Antarctica National Institute of Polar Research Repository, Japan Antarctic
spellingShingle boron
chlorine
Antarctic chondrite
terrestrial contamination
prompt
Oura, Yasuji
Takahashi, Chieko
Ebihara, Mitsuru
Boron and chlorine abundances in Antarctic chondrites: A PGA study
title Boron and chlorine abundances in Antarctic chondrites: A PGA study
title_full Boron and chlorine abundances in Antarctic chondrites: A PGA study
title_fullStr Boron and chlorine abundances in Antarctic chondrites: A PGA study
title_full_unstemmed Boron and chlorine abundances in Antarctic chondrites: A PGA study
title_short Boron and chlorine abundances in Antarctic chondrites: A PGA study
title_sort boron and chlorine abundances in antarctic chondrites: a pga study
topic boron
chlorine
Antarctic chondrite
terrestrial contamination
prompt
topic_facet boron
chlorine
Antarctic chondrite
terrestrial contamination
prompt
url https://nipr.repo.nii.ac.jp/record/6049/files/KJ00002352177.pdf
https://doi.org/10.15094/00006049
https://nipr.repo.nii.ac.jp/records/6049