ログイン
言語:

WEKO3

  • トップ
  • ランキング
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": "9e77ced8-085c-4a6b-bc09-755acdecf9ca"}, "_deposit": {"id": "12038", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "12038"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00012038", "sets": []}, "author_link": ["36897", "36898", "36899"], "item_10_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1999-03-23", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "106", "bibliographicPageStart": "87", "bibliographicVolumeNumber": "33", "bibliographic_titles": [{"bibliographic_title": "信州大学理学部紀要"}]}]}, "item_10_description_20": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The Omine Belt (Kosaka et al. 1979) is lying from Otari to Matsumoto with 65km in length and 5~7km in width along the Itoigawa-Shizuoka Tectonic Line, which is the western manginal fault of the Fossa Magna region. The Omine Belt is burried up by a large amount of non-marine normal clastic and volcaniclastic sediments which ranges in age from Pliocene to early Pleistocene. Plio-Pleistocene strata in the Omine Belt are divided into the Otari and Omine Formations in ascending order. Volcaniclastic sediments of the Otari Formation are andesitic. On the other hand, most of volcaniclastic sediments of the Omine Formation are acidic. In this paper, acidic volcaniclastic sediments are collected and analised in petrographically. 9 samples of the Otari Formation and 64 samples of the Omine Formation are analised. The results are as follows 1) Acidic volcaniclastic sediments in the Omine Belt are made up largely by pumiceous vitric tuff and welded tuff in lithologically. 2) Most of welded tuff beds are rhyolitic petrologically in which biotite occur as main heavy minerals. 3) The Takagariyama tuff I ・ II, which are characterized by a dominance of orthorhombic pyroxene as heavy minerals, are correlative to the Nyukawa Pyroclastic Flow Deposits and Ebisutoge Pyroclastic Deposits in the Takayama Basin, west of Japan Alpus.", "subitem_description_type": "Abstract"}]}, "item_10_description_30": {"attribute_name": "資源タイプ(コンテンツの種類)", "attribute_value_mlt": [{"subitem_description": "Article", "subitem_description_type": "Other"}]}, "item_10_description_31": {"attribute_name": "フォーマット:mimeタイプ", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_10_description_5": {"attribute_name": "引用", "attribute_value_mlt": [{"subitem_description": "信州大学理学部紀要 33(2): 87-106(1999)", "subitem_description_type": "Other"}]}, "item_10_publisher_4": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "信州大学理学部"}]}, "item_10_select_64": {"attribute_name": "著者版フラグ", "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": "PISSN"}]}, "item_10_source_id_39": {"attribute_name": "NII ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0583-063X", "subitem_source_identifier_type": "PISSN"}]}, "item_10_source_id_40": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AA00697923", "subitem_source_identifier_type": "NCID"}]}, "item_10_text_66": {"attribute_name": "sortkey", "attribute_value_mlt": [{"subitem_text_value": "02"}]}, "item_1627890569677": {"attribute_name": "出版タイプ", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "HIBI,  Nobuko", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "36897", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "KOSAKA,  Tomoyoshi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "36898", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "NAGAHASHI,  Yoshitaka", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "36899", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "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": "Science33-02-02.pdf", "filesize": [{"value": "1.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 1100000.0, "url": {"label": "Science33-02-02.pdf", "url": "https://soar-ir.repo.nii.ac.jp/record/12038/files/Science33-02-02.pdf"}, "version_id": "a7d2dd58-f579-4d97-8482-bbbe343de89a"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Petrographic properties of the acidic volcaniclastic deposits in the Omine Belt, western margin of the northern Fossa Magna region, central Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Petrographic properties of the acidic volcaniclastic deposits in the Omine Belt, western margin of the northern Fossa Magna region, central Japan", "subitem_title_language": "en"}]}, "item_type_id": "10", "owner": "1", "path": ["1186"], "permalink_uri": "http://hdl.handle.net/10091/10653", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2010-10-06"}, "publish_date": "2010-10-06", "publish_status": "0", "recid": "12038", "relation": {}, "relation_version_is_last": true, "title": ["Petrographic properties of the acidic volcaniclastic deposits in the Omine Belt, western margin of the northern Fossa Magna region, central Japan"], "weko_shared_id": -1}
  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 33

Petrographic properties of the acidic volcaniclastic deposits in the Omine Belt, western margin of the northern Fossa Magna region, central Japan

http://hdl.handle.net/10091/10653
http://hdl.handle.net/10091/10653
2caafe99-6716-4f58-b615-ef882f8a9390
名前 / ファイル ライセンス アクション
Science33-02-02.pdf Science33-02-02.pdf (1.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-10-06
タイトル
言語 en
タイトル Petrographic properties of the acidic volcaniclastic deposits in the Omine Belt, western margin of the northern Fossa Magna region, central Japan
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 HIBI, Nobuko

× HIBI, Nobuko

WEKO 36897

en HIBI, Nobuko

Search repository
KOSAKA, Tomoyoshi

× KOSAKA, Tomoyoshi

WEKO 36898

en KOSAKA, Tomoyoshi

Search repository
NAGAHASHI, Yoshitaka

× NAGAHASHI, Yoshitaka

WEKO 36899

en NAGAHASHI, Yoshitaka

Search repository
出版者
出版者 信州大学理学部
引用
内容記述タイプ Other
内容記述 信州大学理学部紀要 33(2): 87-106(1999)
書誌情報 信州大学理学部紀要

巻 33, 号 2, p. 87-106, 発行日 1999-03-23
抄録
内容記述タイプ Abstract
内容記述 The Omine Belt (Kosaka et al. 1979) is lying from Otari to Matsumoto with 65km in length and 5~7km in width along the Itoigawa-Shizuoka Tectonic Line, which is the western manginal fault of the Fossa Magna region. The Omine Belt is burried up by a large amount of non-marine normal clastic and volcaniclastic sediments which ranges in age from Pliocene to early Pleistocene. Plio-Pleistocene strata in the Omine Belt are divided into the Otari and Omine Formations in ascending order. Volcaniclastic sediments of the Otari Formation are andesitic. On the other hand, most of volcaniclastic sediments of the Omine Formation are acidic. In this paper, acidic volcaniclastic sediments are collected and analised in petrographically. 9 samples of the Otari Formation and 64 samples of the Omine Formation are analised. The results are as follows 1) Acidic volcaniclastic sediments in the Omine Belt are made up largely by pumiceous vitric tuff and welded tuff in lithologically. 2) Most of welded tuff beds are rhyolitic petrologically in which biotite occur as main heavy minerals. 3) The Takagariyama tuff I ・ II, which are characterized by a dominance of orthorhombic pyroxene as heavy minerals, are correlative to the Nyukawa Pyroclastic Flow Deposits and Ebisutoge Pyroclastic Deposits in the Takayama Basin, west of Japan Alpus.
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 PISSN
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 AA00697923
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 11:36:21.304171
Show All versions

Share

Mendeley Twitter Facebook Print Addthis

Cite as

エクスポート

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

Confirm


Powered by WEKO3


Powered by WEKO3