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Chemical composition and fission-track age of some Muoug Nong-type tektites
https://nipr.repo.nii.ac.jp/records/1387
https://nipr.repo.nii.ac.jp/records/138712397582-77e7-4880-9dfc-3159783ecbe7
名前 / ファイル | ライセンス | アクション |
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KJ00000012021 (1.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1982-12-01 | |||||
タイトル | ||||||
タイトル | Chemical composition and fission-track age of some Muoug Nong-type tektites | |||||
言語 | en | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Yagi, Kenzo
× Yagi, Kenzo× Kuroda, Yoshimasu× Koshimizu, Satoshi |
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著者所属(英) | ||||||
言語 | en | |||||
値 | Hokusei Gakuen College | |||||
著者所属(英) | ||||||
言語 | en | |||||
値 | Department of Geology, Faculty of Science, Shinsyu University | |||||
著者所属(英) | ||||||
言語 | en | |||||
値 | Department of Geology and Mineralogy, Faculty of Science, Hokkaido University | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Six Muong Nong-type tektites from Laos and Thailand and one indochinite from Viet Nam were studied petrologically, and their fission-track age was determined. Under the microscope the tektites have conspicuous flow structures, formed by alternating bands of glass of slightly different refractive index. In one sample B, pale brown parts are present sporadically in the colorless matrix, and both of them show some difference in chemical composition. Major elements were determined by a Hitachi scanning electron probe microanalyzer. It is remarkable that there is a wide range in chemical composition of Muong Nong-type tektites, ranging from 71 to 82% SiO_2,which almost covers the whole range of tektites in general. For determination of water content, a finely powdered sample was melted in a high-frequency induction furnace in vacuum, and evolved water was converted to hydrogen. Water content was determined by measuring the volume of the hydrogen, and the isotopic composition of the hydrogen was determined by a mass spectrometer MAT 250. H_2O content ranges from 0.08 to 0.10%, and δD from -56.4 to -79.2‰. These values preclude the possibility that the water was derived from the lunar rocks, but may support the terrestrial origin of these tektites. Fission-track age dating gives values from 0.65 to 0.70 Ma, which agree with the ages obtained by other workers using fission-track and other methods on the indochinites in general. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 25, p. 162-170, 発行日 1982-12 |