ログイン
言語:

WEKO3

  • トップ
  • コミュニティ
  • ランキング
AND
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

{"_buckets": {"deposit": "41dc9011-8629-40ed-9b0b-d9b2dfa27abb"}, "_deposit": {"id": "16988", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "16988"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00016988", "sets": []}, "author_link": ["48568", "48569", "48570"], "item_11_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\uff08\u5225\u8a00\u8a9e\u7b49\uff09\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "On the Microscopic Pyrites in the N eogene Marine Sediments in Ueda region\uff0cNagano Prefecture\uff0cCe ntral Japan"}]}, "item_11_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1989-03-31", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "42", "bibliographicPageStart": "33", "bibliographicVolumeNumber": "11", "bibliographic_titles": [{"bibliographic_title": "\u74b0\u5883\u79d1\u5b66\u5e74\u5831"}]}]}, "item_11_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The microscopic pyrite occures in the bluish gray mudstones\uff0cb luish gray sandstones or the black shales. Scanning electron microscope observations have shown that there are various forms of pyrites in Ogawa-\uff0cBessho-\uff0cAoki-\uff0ca 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\uff0coctaherdron and pentagonal dodecahedron. The framboidal pyrites were composed of various shapes of single crystals. The crystal habits of microcrystals forming the framboids were octahedron\uff0ch exoctahedron and pentagonal dodecahedron. The framboids have various diameters ranging from 2t o 100um\uff0cho wever\uff0cthese 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\uff0con the other hand\uff0cwere 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\uff0csa ndstone and shale in the Ueda region", "subitem_description_type": "Abstract"}]}, "item_11_description_30": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7\uff08\u30b3\u30f3\u30c6\u30f3\u30c4\u306e\u7a2e\u985e\uff09", "attribute_value_mlt": [{"subitem_description": "Article", "subitem_description_type": "Other"}]}, "item_11_description_31": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8\uff1amime\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_11_description_5": {"attribute_name": "\u5f15\u7528", "attribute_value_mlt": [{"subitem_description": "\u74b0\u5883\u79d1\u5b66\u5e74\u583111:33-42(1989)", "subitem_description_type": "Other"}]}, "item_11_link_3": {"attribute_name": "\u4fe1\u5dde\u5927\u5b66\u7814\u7a76\u8005\u7dcf\u89a7\u3078\u306e\u30ea\u30f3\u30af", "attribute_value_mlt": [{"subitem_link_text": "\u85e4\u677e, \u4ec1", "subitem_link_url": "http://soar-rd.shinshu-u.ac.jp/profile/ja.gCSNjekV.html"}]}, "item_11_publisher_4": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "\u4fe1\u5dde\u5927\u5b66\u74b0\u5883\u79d1\u5b66\u7814\u7a76\u4f1a"}]}, "item_11_select_64": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_11_source_id_35": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0915-7492", "subitem_source_identifier_type": "ISSN"}]}, "item_11_source_id_39": {"attribute_name": "NII ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0915-7492", "subitem_source_identifier_type": "ISSN"}]}, "item_11_source_id_40": {"attribute_name": "\u66f8\u8a8c\u30ec\u30b3\u30fc\u30c9ID", "attribute_value_mlt": [{"subitem_source_identifier": "AN1054947X", "subitem_source_identifier_type": "NCID"}]}, "item_11_text_66": {"attribute_name": "sortkey", "attribute_value_mlt": [{"subitem_text_value": "06"}]}, "item_1627890728808": {"attribute_name": "\u51fa\u7248\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "\u77e2\u5f66\u6ca2,  \u6e05\u5141"}], "nameIdentifiers": [{"nameIdentifier": "48568", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u4e0a\u91ce,  \u6e80\u592b"}], "nameIdentifiers": [{"nameIdentifier": "48569", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u85e4\u677e,  \u4ec1"}], "nameIdentifiers": [{"nameIdentifier": "48570", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2015-09-28"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "11-07.pdf", "filesize": [{"value": "821.0 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 821000.0, "url": {"label": "11-07.pdf", "url": "https://soar-ir.repo.nii.ac.jp/record/16988/files/11-07.pdf"}, "version_id": "0ff647e7-3008-4836-a4aa-1051a606f1f3"}]}, "item_keyword": {"attribute_name": "\u30ad\u30fc\u30ef\u30fc\u30c9", "attribute_value_mlt": [{"subitem_subject": "neogene marine sediment", "subitem_subject_scheme": "Other"}, {"subitem_subject": "microscopic pyrite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "framboidal pyrite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "single euhedral pyrite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u65b0\u7b2c\u4e09\u7d00\u6d77\u6210\u5806\u7a4d\u7269", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u5fae\u5c0f\u30d1\u30a4\u30e9\u30a4\u30c8", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u30d5\u30e9\u30f3\u30dc\u30a4\u30c0\u30eb\u30d1\u30a4\u30e9\u30a4\u30c8", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u5358\u4e00\u767d\u5f62\u30d1\u30a4\u30e9\u30a4\u30c8", "subitem_subject_scheme": "Other"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "jpn"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "research report", "resourceuri": "http://purl.org/coar/resource_type/c_18ws"}]}, "item_title": "\u4e0a\u7530\u5730\u65b9\u306e\u65b0\u7b2c\u4e09\u7d00\u6d77\u6210\u5806\u7a4d\u7269\u4e2d\u306b\u898b\u51fa\u3055\u308c\u308b\u5fae\u5c0f\u30d1\u30a4\u30e9\u30a4\u30c8\u306b\u3064\u3044\u3066", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "\u4e0a\u7530\u5730\u65b9\u306e\u65b0\u7b2c\u4e09\u7d00\u6d77\u6210\u5806\u7a4d\u7269\u4e2d\u306b\u898b\u51fa\u3055\u308c\u308b\u5fae\u5c0f\u30d1\u30a4\u30e9\u30a4\u30c8\u306b\u3064\u3044\u3066", "subitem_title_language": "ja"}]}, "item_type_id": "11", "owner": "1", "path": ["1628/1629/1659"], "permalink_uri": "http://hdl.handle.net/10091/12677", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2011-04-19"}, "publish_date": "2011-04-19", "publish_status": "0", "recid": "16988", "relation": {}, "relation_version_is_last": true, "title": ["\u4e0a\u7530\u5730\u65b9\u306e\u65b0\u7b2c\u4e09\u7d00\u6d77\u6210\u5806\u7a4d\u7269\u4e2d\u306b\u898b\u51fa\u3055\u308c\u308b\u5fae\u5c0f\u30d1\u30a4\u30e9\u30a4\u30c8\u306b\u3064\u3044\u3066"], "weko_shared_id": -1}
  1. 900 信州大学刊行物
  2. 信州大学 環境科学年報
  3. Vol. 11

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
11-07.pdf 11-07.pdf (821.0 kB)
Item type 研究報告書 / Research Paper(1)
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

WEKO 48568

矢彦沢, 清允

Search repository
上野, 満夫

× 上野, 満夫

WEKO 48569

上野, 満夫

Search repository
藤松, 仁

× 藤松, 仁

WEKO 48570

藤松, 仁

Search repository
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
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
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 09:46:20.293682
Show All versions

Share

Mendeley CiteULike Twitter Facebook Print Addthis

Cite as

Export

OAI-PMH
  • OAI-PMH JPCOAR
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by CERN Data Centre & Invenio


Powered by CERN Data Centre & Invenio