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Thermoluminescence characteristics and chemical compositions of mesostases in ordinary chondrites
https://doi.org/10.15094/00004552
https://doi.org/10.15094/00004552a80c21eb-e268-44dd-b589-cea5b397d962
名前 / ファイル | ライセンス | アクション |
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KJ00000036358 (903.2 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1991-03-01 | |||||
タイトル | ||||||
タイトル | Thermoluminescence characteristics and chemical compositions of mesostases in ordinary chondrites | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00004552 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Ninagawa,Kiyotaka
× Ninagawa,Kiyotaka× Kubo,Hideyuki× Fujimura,Shin-ichi× Yamamoto, Isao× Wada,Tomonori× Matsunami,Satoshi× Nishimura,Hiroshi |
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著者所属(英) | ||||||
en | ||||||
Okayama University of Science/Okayama University of Science/ Okayama University of Science/Okayama University of Science/ Okayama University/Naruto University of Education/Naruto University of Education | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Induced thermoluminescence (TL) images of ordinary chondrites, ALH-77214 (L3.4-3.5), Y-74191 (L3.6), ALH-77216 (L3.8) and ALH-78043 (L6), were measured by the TL spatial distribution readout system combined with a microscope and TL characteristics [peak temperature and peak width] of mesostases were analyzed. Their chemical compositions were also analyzed by an electron probe X-ray microanalyzer. We found that; (1) The mesostasis was responsible for much of the TL in the ordinary chondrites, (2) A mesostasis of normative anorthite compositions showed low peak temperature (∿90℃) and narrow width (∿65℃), while a mesostasis of normative albite compositions showed high peak temperature (∿125℃) and wide width (∿100℃), (3) A main phosphor in a low petrologic grade chondrite <3.5 was a high anorthite mesostasis and that in high grade chondrites >3.5 was a high albite mesostasis, (4) Some chondrules in the same fragments of the type 3 chondrites showed no or weak TL emission and these mesostases had high normative albite. These facts suggest that in type 3 ordinary chondrites; (1) The post-accretional metamorphism cannot account for the coexistence of high albite mesostases with TL emission and no emission and a high anorthite mesostasis with TL emission, (2) Low petrologic grade chondrites <3.5 have a large population of rapidly cooled chondrules and high petrologic grade chondrites >3.5 have a large population of slowly cooled chondrules. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10784627 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Meteorites 巻 4, p. 344-351, 発行日 1991-03 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |