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Crystallinity indices of quartz in chert of Central Japan: their reliability and some geological applications
http://hdl.handle.net/10098/2116
http://hdl.handle.net/10098/211604150ae4-4cf7-4477-a2d8-62df678a5442
名前 / ファイル | ライセンス | アクション |
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Bulletin_of_Fuku_City_Museum_of_Natural_History55.pdf (3.6 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2009-07-30 | |||||
タイトル | ||||||
タイトル | Crystallinity indices of quartz in chert of Central Japan: their reliability and some geological applications | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 中部日本のチャート中の石英の結晶度:その信頼性および地質学的応用 | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | crystallinity index | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | quartz | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | chert | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | diagenesis | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | provenance | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | thermal | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | effect | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | XRD | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 結晶度 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 石英 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | チャート | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 続成過程 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 供給地 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 熱史 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | X線解析 | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_1843 | |||||
資源タイプ | other | |||||
著者 |
HATTORI, Isamu
× HATTORI, Isamu× UMEDA, Miyuki× 服部, 勇× 梅田, 美由紀 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Crystallinity indices of quartz(CI) determined by X-ray analysis have been reported in various types of chert of different ages. Reported CI's distribute from <1 to 10. The difference may result from the difference in sample state prepared for determination of CI or existence of essential variation in crystallinity of quartz. We determined CI of many euhedral quartz crystals and quartz in cherts in different sample states, and could conclude that CI does not depend largely on sample states prepared with different methods, but depends partially on euhedral macroquartz used as a standard material. Even after removing this disadvantage, there is still wide difference in CI of quartz, indicating that CI is not uniform but varies according to the mode of origin and the thermal processes having operated on the quartz. Our data coupled with data described in literature show that 1) CI's in Cenozoic deep-sea oozes and cherts are lower than those in Mesozoic bedded chertz on land, 2) bedded cherts suffering thermal effect are characterized by higher CI, 3) CI's lacustrine and fluvial cherts are higher than those of bedded cherts of deep-sea origin, 4) CI's of older cherts are generally larger than those of younger cherts of the similar origin. This analysis suggests that CI can be used as a useful indicator deciphering origin of sedimentary siliceous rocks and their diagenetic and metamorphic stages. | |||||
書誌情報 |
Bulletin of Fukui City Museum of Natural History 号 55, p. 17-32, 発行日 2008-12 |
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出版者 | ||||||
出版者 | 福井市自然史博物館 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 9199691 | |||||
書誌レコードID | ||||||
識別子タイプ | NCID | |||||
関連識別子 | TD00007353 | |||||
著者版フラグ | ||||||
出版タイプ | AO | |||||
出版タイプResource | http://purl.org/coar/version/c_b1a7d7d4d402bcce |