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"Other"}, {"subitem_subject": "微小パイラト", "subitem_subject_scheme": "Other"}, {"subitem_subject": "フランボイダルパイライト", "subitem_subject_scheme": "Other"}, {"subitem_subject": "フランボイ夕ル褐鉄鉱", "subitem_subject_scheme": "Other"}, {"subitem_subject": "単一自形パイライト", "subitem_subject_scheme": "Other"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "jpn"}]}, "item_resource_type": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"resourcetype": "research report", "resourceuri": "http://purl.org/coar/resource_type/c_18ws"}]}, "item_title": "松本北東地域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", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "松本北東地域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", "subitem_title_language": "ja"}, {"subitem_title": "On the Microscopic Pyrite in the Neogene Marine Sediments in the north -eastern Matsumoto Region,Nagano Prefecture,Central Japan", "subitem_title_language": "en"}]}, "item_type_id": "11", "owner": "1", "path": 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松本北東地域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/10091/12544
http://hdl.handle.net/10091/12544bfcebc59-0e5c-4153-a6ae-4b769f5bcbac
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 | 松本北東地域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 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | On the Microscopic Pyrite in the Neogene Marine Sediments in the north -eastern Matsumoto Region,Nagano Prefecture,Central Japan | |||||
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 | framboidal limonite | |||||
キーワード | ||||||
主題 | single eduhedral 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 | フランボイ夕ル褐鉄鉱 | |||||
キーワード | ||||||
主題 | 単一自形パイライト | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_18ws | |||||
タイプ | research report | |||||
著者 |
矢彦沢, 清充
× 矢彦沢, 清充× 加藤, 和彦× 荒井, 智彦× 上野, 満夫× 山本, 満寿夫× 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13:114-122(1991) | |||||
書誌情報 |
環境科学年報 巻 13, p. 114-122, 発行日 1991-03-31 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The microscopic pyrite is most frequently found in the gray mudstone,gray sandstone and black shales which occur at Bessho-,Aoki-,a nd Uchimura formation in the north -eastern Matsumoto region. Forms and shapes of the pyrites have been investigated by electron microscopic measurements_ The pyrites were made up of spherical aggregates of microcrystals termed framboid and single euhedral crystal containing mainly octahedron and truncated octahedron. The framboidal pyrites were composed of various shapes of single crystals. The crystal habits of microcrystals forming the framboids were octahedron and truncated octahedron. The framboids have various diameters ranging from 1 to 60um. The diameters of the microcrystals contained in the framboids were in various sizes fromO.5 to 5um,a nd it seems that the diameter of microcrystals increases with the diameter of framboids. Pyrite -sulfur of the unweatherd mudstone, sandstone and shale is contained in the range of 0.01 -1% . Framboids in the weatherd mudstone,sandstone and shales are composed of the limonite. The occurrence of microscopic pyrite suggests sign of strong reduction of resediment at the early stage of diagenesis of mudstone,sandstone and .shale in the north - eastern Matsumoto 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 |