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": "a473baa8-6f9e-407c-9c63-2524c4a2eba4"}, "_deposit": {"id": "19800", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "19800"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00019800"}, "item_10_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": "Paleosols in the lower part of the Seto Group, Ena City, Gifu Prefecture, central Japan"}]}, "item_10_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2018-03-30", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "43", "bibliographicPageStart": "25", "bibliographicVolumeNumber": "47", "bibliographic_titles": [{"bibliographic_title": "Journal of the Faculty of Science Shinshu University"}]}]}, "item_10_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The Paleopedological and sedimentological studies were carried out with clay mineralogy on the middle Miocene Tokiguchi Porcelain Clay Formation distributed in Hara Mine in Yamaoka-cho, Ena City, Gifu Prefecture, central Japan. The main part of the Tokiguchi Porcelain Clay Formation,which mainly consists of clay-sized sediments with the alternation of sand and silt sediments,was deposited in stagnant water condition situated in lacustrine environment. The coarse debris flow deposits, however, were predominant in the marginal area of the basin. This wide variety of sedimentary facies is indicative of the diverse and highly undulated morphology.\nThe immature paleosol correlatable to inceptisol, which was intercalated in the debris flow deposits that buried the standing tree trunks,was formed in the marginal area of the sedimentary basin.The mature paleosol correlatable to ultisol was predominant on the emerged lake deposits.These suggest that the whole area of the sedimentary basin was situated by a large fluctuation of the lake water level and ground water table.", "subitem_description_type": "Abstract"}]}, "item_10_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_10_description_5": {"attribute_name": "\u5f15\u7528", "attribute_value_mlt": [{"subitem_description": "Journal of the Faculty of Science Shinshu University 47 :  25-43(2018)", "subitem_description_type": "Other"}]}, "item_10_publisher_4": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "The Faculty of Science, Shinshu University"}]}, "item_10_select_64": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_10_source_id_35": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0583-063X", "subitem_source_identifier_type": "ISSN"}]}, "item_10_source_id_39": {"attribute_name": "NII ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0583-063X", "subitem_source_identifier_type": "ISSN"}]}, "item_10_source_id_40": {"attribute_name": "\u66f8\u8a8c\u30ec\u30b3\u30fc\u30c9ID", "attribute_value_mlt": [{"subitem_source_identifier": "AA00697924", "subitem_source_identifier_type": "NCID"}]}, "item_10_text_66": {"attribute_name": "sortkey", "attribute_value_mlt": [{"subitem_text_value": "03"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "\u8449\u7530\u91ce, \u5e0c"}], "nameIdentifiers": [{"nameIdentifier": "105480", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u5165\u6c5f, \u5fd7\u7e54"}], "nameIdentifiers": [{"nameIdentifier": "105481", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u5409\u7530, \u5b5d"}], "nameIdentifiers": [{"nameIdentifier": "105482", "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": "2018-04-23"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "Science47-03.pdf", "filesize": [{"value": "2.2 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 2200000.0, "url": {"label": "Science47-03.pdf", "url": "https://soar-ir.repo.nii.ac.jp/record/19800/files/Science47-03.pdf"}, "version_id": "8f3a246f-5d77-4b17-8288-4c3bf04ef21a"}]}, "item_keyword": {"attribute_name": "\u30ad\u30fc\u30ef\u30fc\u30c9", "attribute_value_mlt": [{"subitem_subject": "\u702c\u6238\u5c64\u7fa4", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u4e2d\u90e8\u4e2d\u65b0\u7d71", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u53e4\u571f\u58cc", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u5806\u7a4d\u76f8\u89e3\u6790", "subitem_subject_scheme": "Other"}, {"subitem_subject": "\u7c98\u571f\u9271\u7269\u7d44\u6210", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Seto Group", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Middle Miocene", "subitem_subject_scheme": "Other"}, {"subitem_subject": "paleosol", "subitem_subject_scheme": "Other"}, {"subitem_subject": "sedimentary facies analysis", "subitem_subject_scheme": "Other"}, {"subitem_subject": "clay mineral assemblage", "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": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "\u5c90\u961c\u770c\u6075\u90a3\u5e02\u306b\u5206\u5e03\u3059\u308b\u702c\u6238\u5c64\u7fa4\u4e0b\u90e8\u5c64\u306e\u53e4\u571f\u58cc", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "\u5c90\u961c\u770c\u6075\u90a3\u5e02\u306b\u5206\u5e03\u3059\u308b\u702c\u6238\u5c64\u7fa4\u4e0b\u90e8\u5c64\u306e\u53e4\u571f\u58cc"}]}, "item_type_id": "10", "owner": "1", "path": ["1169/1171/1172/1881"], "permalink_uri": "http://hdl.handle.net/10091/00020561", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_value": "2018-04-23"}, "publish_date": "2018-04-23", "publish_status": "0", "recid": "19800", "relation": {}, "relation_version_is_last": true, "title": ["\u5c90\u961c\u770c\u6075\u90a3\u5e02\u306b\u5206\u5e03\u3059\u308b\u702c\u6238\u5c64\u7fa4\u4e0b\u90e8\u5c64\u306e\u53e4\u571f\u58cc"], "weko_shared_id": null}
  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 47

岐阜県恵那市に分布する瀬戸層群下部層の古土壌

http://hdl.handle.net/10091/00020561
1c353859-b522-4a87-9b72-cfe65371ca93
名前 / ファイル ライセンス アクション
Science47-03.pdf Science47-03.pdf (2.2 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2018-04-23
タイトル
タイトル 岐阜県恵那市に分布する瀬戸層群下部層の古土壌
言語
言語 jpn
キーワード
主題Scheme Other
主題 瀬戸層群
キーワード
主題Scheme Other
主題 中部中新統
キーワード
主題Scheme Other
主題 古土壌
キーワード
主題Scheme Other
主題 堆積相解析
キーワード
主題Scheme Other
主題 粘土鉱物組成
キーワード
主題Scheme Other
主題 Seto Group
キーワード
主題Scheme Other
主題 Middle Miocene
キーワード
主題Scheme Other
主題 paleosol
キーワード
主題Scheme Other
主題 sedimentary facies analysis
キーワード
主題Scheme Other
主題 clay mineral assemblage
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
その他(別言語等)のタイトル
その他のタイトル Paleosols in the lower part of the Seto Group, Ena City, Gifu Prefecture, central Japan
著者 葉田野, 希

× 葉田野, 希

WEKO 105480

葉田野, 希

Search repository
入江, 志織

× 入江, 志織

WEKO 105481

入江, 志織

Search repository
吉田, 孝

× 吉田, 孝

WEKO 105482

吉田, 孝

Search repository
出版者
出版者 The Faculty of Science, Shinshu University
引用
内容記述タイプ Other
内容記述 Journal of the Faculty of Science Shinshu University 47 : 25-43(2018)
書誌情報 Journal of the Faculty of Science Shinshu University

巻 47, p. 25-43, 発行日 2018-03-30
抄録
内容記述タイプ Abstract
内容記述 The Paleopedological and sedimentological studies were carried out with clay mineralogy on the middle Miocene Tokiguchi Porcelain Clay Formation distributed in Hara Mine in Yamaoka-cho, Ena City, Gifu Prefecture, central Japan. The main part of the Tokiguchi Porcelain Clay Formation,which mainly consists of clay-sized sediments with the alternation of sand and silt sediments,was deposited in stagnant water condition situated in lacustrine environment. The coarse debris flow deposits, however, were predominant in the marginal area of the basin. This wide variety of sedimentary facies is indicative of the diverse and highly undulated morphology.
The immature paleosol correlatable to inceptisol, which was intercalated in the debris flow deposits that buried the standing tree trunks,was formed in the marginal area of the sedimentary basin.The mature paleosol correlatable to ultisol was predominant on the emerged lake deposits.These suggest that the whole area of the sedimentary basin was situated by a large fluctuation of the lake water level and ground water table.
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 0583-063X
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00697924
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 08:32:08.870987
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