Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites

Mineralogy of fine-grained matrix (FGM), fine-grained rim (FGR), chondrule rim, and altered mesostasis of a chondrule from the Asuka (A) 12169 CM3.0 chondrite was investigated by field emission scanning electron microscopy (FE-SEM), synchrotron radiation-based X-ray nano-tomography (SR-XCT), and tra...

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Published in:Polar Science
Main Authors: Noguchi, Takaaki, Yasutake, Masahiro, Tsuchiyama, Akira, Miyake, Akira, Kimura, Makoto, Yamaguchi, Akira, Imae, Naoya, Uesugi, Kentaro, Takeuchi, Akihisa
Language:English
Published: 2021
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/records/16836
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author Noguchi, Takaaki
Yasutake, Masahiro
Tsuchiyama, Akira
Miyake, Akira
Kimura, Makoto
Yamaguchi, Akira
Imae, Naoya
Uesugi, Kentaro
Takeuchi, Akihisa
author_facet Noguchi, Takaaki
Yasutake, Masahiro
Tsuchiyama, Akira
Miyake, Akira
Kimura, Makoto
Yamaguchi, Akira
Imae, Naoya
Uesugi, Kentaro
Takeuchi, Akihisa
author_sort Noguchi, Takaaki
collection National Institute of Polar Research Repository, Japan
container_start_page 100727
container_title Polar Science
container_volume 29
description Mineralogy of fine-grained matrix (FGM), fine-grained rim (FGR), chondrule rim, and altered mesostasis of a chondrule from the Asuka (A) 12169 CM3.0 chondrite was investigated by field emission scanning electron microscopy (FE-SEM), synchrotron radiation-based X-ray nano-tomography (SR-XCT), and transmission electron microscopy (TEM). SR-XCT and TEM observations revealed that both FGM and FGR contain abundant amorphous silicate embedding nano-inclusions (most are Fe–Ni sulfide). Although the amorphous silicate is more or less hydrated based on the analysis of the X-ray linear attenuation coefficients in SR-XCT, there are no areas filled by abundant phyllosilicate even in three dimensions. However, FGM and FGR contain ~2-10 μm-sized aggregates composed of tochilinite, nano-inclusions of possible magnetite, and poorly crystalline serpentine without sharp boundaries with the surroundings. It is unlikely that the heterogeneity resulted from brecciation and mixing of materials that experienced different degrees of aqueous alteration, but more likely from a very early stage of aqueous alteration that proceeded heterogeneously depending on locally different chemistry. Chondrule mesostasis near the surface of a chondrule was altered to saponite with tochilinite-rich aggregates. These observations indicate that the degree aqueous alteration of A 12169 is very low and that it is comparable with that of Acfer 094, ALH 77307, and the least altered areas of Paris. journal article
genre Polar Science
Polar Science
genre_facet Polar Science
Polar Science
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institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.1016/j.polar.2021.100727
op_relation 10.1016/j.polar.2021.100727
https://doi.org/10.1016/j.polar.2021.100727
Polar Science
29
100727
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https://nipr.repo.nii.ac.jp/records/16836
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00016836 2025-04-13T14:25:55+00:00 Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites Noguchi, Takaaki Yasutake, Masahiro Tsuchiyama, Akira Miyake, Akira Kimura, Makoto Yamaguchi, Akira Imae, Naoya Uesugi, Kentaro Takeuchi, Akihisa 2021-09 https://nipr.repo.nii.ac.jp/records/16836 eng eng 10.1016/j.polar.2021.100727 https://doi.org/10.1016/j.polar.2021.100727 Polar Science 29 100727 18739652 https://nipr.repo.nii.ac.jp/records/16836 metadata only access CM chondrite Subtype 3.0 Amorphous silicate Enstatite whisker Nano-tomography 2021 ftnipr https://doi.org/10.1016/j.polar.2021.100727 2025-03-19T10:19:56Z Mineralogy of fine-grained matrix (FGM), fine-grained rim (FGR), chondrule rim, and altered mesostasis of a chondrule from the Asuka (A) 12169 CM3.0 chondrite was investigated by field emission scanning electron microscopy (FE-SEM), synchrotron radiation-based X-ray nano-tomography (SR-XCT), and transmission electron microscopy (TEM). SR-XCT and TEM observations revealed that both FGM and FGR contain abundant amorphous silicate embedding nano-inclusions (most are Fe–Ni sulfide). Although the amorphous silicate is more or less hydrated based on the analysis of the X-ray linear attenuation coefficients in SR-XCT, there are no areas filled by abundant phyllosilicate even in three dimensions. However, FGM and FGR contain ~2-10 μm-sized aggregates composed of tochilinite, nano-inclusions of possible magnetite, and poorly crystalline serpentine without sharp boundaries with the surroundings. It is unlikely that the heterogeneity resulted from brecciation and mixing of materials that experienced different degrees of aqueous alteration, but more likely from a very early stage of aqueous alteration that proceeded heterogeneously depending on locally different chemistry. Chondrule mesostasis near the surface of a chondrule was altered to saponite with tochilinite-rich aggregates. These observations indicate that the degree aqueous alteration of A 12169 is very low and that it is comparable with that of Acfer 094, ALH 77307, and the least altered areas of Paris. journal article Other/Unknown Material Polar Science Polar Science National Institute of Polar Research Repository, Japan Polar Science 29 100727
spellingShingle CM chondrite
Subtype 3.0
Amorphous silicate
Enstatite whisker
Nano-tomography
Noguchi, Takaaki
Yasutake, Masahiro
Tsuchiyama, Akira
Miyake, Akira
Kimura, Makoto
Yamaguchi, Akira
Imae, Naoya
Uesugi, Kentaro
Takeuchi, Akihisa
Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites
title Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites
title_full Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites
title_fullStr Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites
title_full_unstemmed Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites
title_short Mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in Asuka 12169, one of the least altered CM chondrites
title_sort mineralogy of fine-grained matrix, fine-grained rim, chondrule rim, and altered mesostasis of a chondrule in asuka 12169, one of the least altered cm chondrites
topic CM chondrite
Subtype 3.0
Amorphous silicate
Enstatite whisker
Nano-tomography
topic_facet CM chondrite
Subtype 3.0
Amorphous silicate
Enstatite whisker
Nano-tomography
url https://nipr.repo.nii.ac.jp/records/16836