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上田地方の新第三紀海成堆積物中に見出される微小パイライトについて
http://hdl.handle.net/10091/12677
9eb423f0-e3e8-42fb-86a9-9fa411abdbd4
名前 / ファイル | ライセンス | アクション | |
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Item type | 研究報告書 / Research Paper(1) | |||||
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公開日 | 2011-04-19 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 上田地方の新第三紀海成堆積物中に見出される微小パイライトについて | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | neogene marine sediment | |||||
キーワード | ||||||
主題 | microscopic pyrite | |||||
キーワード | ||||||
主題 | framboidal pyrite | |||||
キーワード | ||||||
主題 | single euhedral pyrite | |||||
キーワード | ||||||
主題 | 新第三紀海成堆積物 | |||||
キーワード | ||||||
主題 | 微小パイライト | |||||
キーワード | ||||||
主題 | フランボイダルパイライト | |||||
キーワード | ||||||
主題 | 単一白形パイライト | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_18ws | |||||
タイプ | research report | |||||
その他(別言語等)のタイトル | ||||||
その他のタイトル | On the Microscopic Pyrites in the N eogene Marine Sediments in Ueda region,Nagano Prefecture,Ce ntral Japan | |||||
著者 |
矢彦沢, 清允
× 矢彦沢, 清允× 上野, 満夫× 藤松, 仁 |
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信州大学研究者総覧へのリンク | ||||||
氏名 | 藤松, 仁 | |||||
URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.gCSNjekV.html | |||||
出版者 | ||||||
出版者 | 信州大学環境科学研究会 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 環境科学年報11:33-42(1989) | |||||
書誌情報 |
環境科学年報 巻 11, p. 33-42, 発行日 1989-03-31 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The microscopic pyrite occures in the bluish gray mudstones,b luish gray sandstones or the black shales. Scanning electron microscope observations have shown that there are various forms of pyrites in Ogawa-,Bessho-,Aoki-,a nd Uchimura formation in Ueda region. The pyrites were made up of spherical aggregates of microcrystals termed framboid and the single euhedral crystal containing mainly hexahedron,octaherdron and pentagonal dodecahedron. The framboidal pyrites were composed of various shapes of single crystals. The crystal habits of microcrystals forming the framboids were octahedron,h exoctahedron and pentagonal dodecahedron. The framboids have various diameters ranging from 2t o 100um,ho wever,these are concentrated at the lower end of this range. The diameters of the microcrystals contained in the framboids were in various sizes from 0.3 to 5um. The sections of framboid constructed from pentagonal dodecahedral crystals showed ar egular honeycomb-likepattern of hexagons. The single euhedral crystals,on the other hand,were in various sizes from 0.5 to 270um. The occurrence of microscopic pyrite must be a sign of strong reduction of the sediment at the early stage of sedimentation-diagenesis of mudstone,sa ndstone and shale in the Ueda region | |||||
資源タイプ(コンテンツの種類) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0915-7492 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN1054947X | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |