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": "05c559fd-eb5a-4e95-8c2e-be0f647082a6"}, "_deposit": {"id": "3212", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "3212"}, "status": "published"}, "_oai": {"id": "oai:niigata-u.repo.nii.ac.jp:00003212", "sets": ["454", "470"]}, "item_5_alternative_title_1": {"attribute_name": "その他のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "Early Devonian Palaeoscenidiidae (Radiolaria) from the \"Yoshiki Formation\" in the Fukuji area of the Hida-gaien Terrane. central Japan, and its biostratigraphic significance"}]}, "item_5_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2003-11", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "11", "bibliographicPageEnd": "647", "bibliographicPageStart": "635", "bibliographicVolumeNumber": "109", "bibliographic_titles": [{"bibliographic_title": "地質学雑誌"}, {"bibliographic_title": "地質学雑誌", "bibliographic_titleLang": "en"}]}]}, "item_5_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Moderately well-preserved Devonian radiolarians were recovered from the mudstone portion of alternating tuffaceous sandstone and mudstone cropping out along a tributary of the Kanashirozako Valley in the Fukuji area of the Hida-gaien Terrane, central Japan. Float samples of tuffaceous mudstone, which were collected from a riverbed near the outcrop mentioned above, also contain well-preserved Devonian radiolarians. These radiolarian-bearing rocks most likely belong to the Yoshiki Formation, based on lithology. Two assemblages (I and II) are present and contain abundant species of the family Palaeoscenidiidae along with ceratoikiscids and undetermined spumellarians. The rocks containing the two assemblages correlate with the upper half of the lower to middle Emsian (upper Lower Devonian) Trilonche (?) sp. A Zone defined in the Nakahata Formation of the Kurosegawa Terrane. Furthermore, the Yoshiki Formation in the lower reaches of the Ichinotani Valley that yields the Zadrappolus yoshikiensis Assemblage can be correlated with a part of the Pridoli to Pragian (upper Upper Silurian to middle Lower Devonian) Futobari solidus Zone of the Nakahata Formation. Therefore, the Yoshiki Formation is probably Pridoli to early to middle Emsian in age. Stratigraphic relationships between the Yoshiki and Fukuji formations have been poorly understood, due to structural complexities, poor exposures, and the lack of age-determinable fossils. However, microfossil data from these two formations reveal that they are almost contemporaneous. Some past workers have suggested that the Yoshiki Formation is unconformably overlain by the Fukuji Formation, but the presence of an unconformity is not supported by the present study.", "subitem_description_type": "Abstract"}, {"subitem_description": "飛騨外縁帯福地地域に分布する吉城層は,その時代についてオルドビス紀,シルル紀および前期デボン紀と諸説が存在した.また,不整合とされたデボン系福地層との関係も,福地層の層序から問題点が指摘されていた.今回,吉城層の模式均一の谷の西方に位置するカナシロザコの枝沢において,新たに吉城層と考えられる地層の露出を確認した.露頭から採取した凝灰質な砂岩泥岩互層の泥岩部および露頭付近の転石として得られた珪長質な凝灰質泥岩から前期デボン紀Emsianを示す放散虫化石が得られた.従来報告されている吉城層の放散虫化石群集(Zadrappolus yoshikiensis群集)と今回発見された群集から,吉城層の時代は後期シルル紀Pridoliから前期デボン紀Emsianの前期である可能性が高い.この時代論は古城層と福地層がほぼ同時代の地層であることを示す.したがって,両側の接触関係が不整合である可能性は極めて低い.", "subitem_description_type": "Abstract"}]}, "item_5_full_name_3": {"attribute_name": "著者別名", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "41462", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Kurihara, Toshiyuki"}]}]}, "item_5_publisher_7": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "日本地質学会"}]}, "item_5_relation_31": {"attribute_name": "異版である", "attribute_value_mlt": [{"subitem_relation_type": "isVersionOf", "subitem_relation_type_id": {"subitem_relation_type_id_text": "http://ci.nii.ac.jp/naid/110003009767", "subitem_relation_type_select": "URI"}}]}, "item_5_rights_15": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "本文データは学協会の許諾に基づきCiNiiから複製したものである"}]}, "item_5_select_19": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_5_source_id_11": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00141768", "subitem_source_identifier_type": "NCID"}]}, "item_5_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "00167630", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "栗原, 敏之"}], "nameIdentifiers": [{"nameIdentifier": "41461", "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": "2019-07-30"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "110003009767.pdf", "filesize": [{"value": "2.8 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 2800000.0, "url": {"label": "110003009767.pdf", "url": "https://niigata-u.repo.nii.ac.jp/record/3212/files/110003009767.pdf"}, "version_id": "c31b94c4-9439-40e7-8f3c-431a56e8ecef"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "Hida-gaien Terrane", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Fujuji area", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Gifu Prefecture", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Yoshiki Formation", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Devonian", "subitem_subject_scheme": "Other"}, {"subitem_subject": "radiolaria", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Palaeoscenidiidae", "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": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "飛騨外縁帯福地地域の\"吉城層\"から前期デボン紀Palaeoscenidiidae科放散虫化石の発見とその生層序学的意義", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "飛騨外縁帯福地地域の\"吉城層\"から前期デボン紀Palaeoscenidiidae科放散虫化石の発見とその生層序学的意義"}, {"subitem_title": "飛騨外縁帯福地地域の\"吉城層\"から前期デボン紀Palaeoscenidiidae科放散虫化石の発見とその生層序学的意義", "subitem_title_language": "en"}]}, "item_type_id": "5", "owner": "1", "path": ["454", "470"], "permalink_uri": "http://hdl.handle.net/10191/26547", "pubdate": {"attribute_name": "公開日", "attribute_value": "2014-03-19"}, "publish_date": "2014-03-19", "publish_status": "0", "recid": "3212", "relation": {}, "relation_version_is_last": true, "title": ["飛騨外縁帯福地地域の\"吉城層\"から前期デボン紀Palaeoscenidiidae科放散虫化石の発見とその生層序学的意義"], "weko_shared_id": null}
  1. 0 資料タイプ別
  2. 01 学術雑誌論文
  1. 230 大学院自然科学研究科
  2. 10 学術雑誌論文
  3. 10 査読済論文

飛騨外縁帯福地地域の"吉城層"から前期デボン紀Palaeoscenidiidae科放散虫化石の発見とその生層序学的意義

http://hdl.handle.net/10191/26547
http://hdl.handle.net/10191/26547
121646ef-4c13-4e3b-8a2f-0ce2d09ffa7d
名前 / ファイル ライセンス アクション
110003009767.pdf 110003009767.pdf (2.8 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2014-03-19
タイトル
タイトル 飛騨外縁帯福地地域の"吉城層"から前期デボン紀Palaeoscenidiidae科放散虫化石の発見とその生層序学的意義
タイトル
言語 en
タイトル 飛騨外縁帯福地地域の"吉城層"から前期デボン紀Palaeoscenidiidae科放散虫化石の発見とその生層序学的意義
言語
言語 jpn
キーワード
主題Scheme Other
主題 Hida-gaien Terrane
キーワード
主題Scheme Other
主題 Fujuji area
キーワード
主題Scheme Other
主題 Gifu Prefecture
キーワード
主題Scheme Other
主題 Yoshiki Formation
キーワード
主題Scheme Other
主題 Devonian
キーワード
主題Scheme Other
主題 radiolaria
キーワード
主題Scheme Other
主題 Palaeoscenidiidae
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
その他のタイトル
その他のタイトル Early Devonian Palaeoscenidiidae (Radiolaria) from the "Yoshiki Formation" in the Fukuji area of the Hida-gaien Terrane. central Japan, and its biostratigraphic significance
著者 栗原, 敏之

× 栗原, 敏之

WEKO 41461

栗原, 敏之

Search repository
著者別名
識別子 41462
識別子Scheme WEKO
姓名 Kurihara, Toshiyuki
抄録
内容記述タイプ Abstract
内容記述 Moderately well-preserved Devonian radiolarians were recovered from the mudstone portion of alternating tuffaceous sandstone and mudstone cropping out along a tributary of the Kanashirozako Valley in the Fukuji area of the Hida-gaien Terrane, central Japan. Float samples of tuffaceous mudstone, which were collected from a riverbed near the outcrop mentioned above, also contain well-preserved Devonian radiolarians. These radiolarian-bearing rocks most likely belong to the Yoshiki Formation, based on lithology. Two assemblages (I and II) are present and contain abundant species of the family Palaeoscenidiidae along with ceratoikiscids and undetermined spumellarians. The rocks containing the two assemblages correlate with the upper half of the lower to middle Emsian (upper Lower Devonian) Trilonche (?) sp. A Zone defined in the Nakahata Formation of the Kurosegawa Terrane. Furthermore, the Yoshiki Formation in the lower reaches of the Ichinotani Valley that yields the Zadrappolus yoshikiensis Assemblage can be correlated with a part of the Pridoli to Pragian (upper Upper Silurian to middle Lower Devonian) Futobari solidus Zone of the Nakahata Formation. Therefore, the Yoshiki Formation is probably Pridoli to early to middle Emsian in age. Stratigraphic relationships between the Yoshiki and Fukuji formations have been poorly understood, due to structural complexities, poor exposures, and the lack of age-determinable fossils. However, microfossil data from these two formations reveal that they are almost contemporaneous. Some past workers have suggested that the Yoshiki Formation is unconformably overlain by the Fukuji Formation, but the presence of an unconformity is not supported by the present study.
抄録
内容記述タイプ Abstract
内容記述 飛騨外縁帯福地地域に分布する吉城層は,その時代についてオルドビス紀,シルル紀および前期デボン紀と諸説が存在した.また,不整合とされたデボン系福地層との関係も,福地層の層序から問題点が指摘されていた.今回,吉城層の模式均一の谷の西方に位置するカナシロザコの枝沢において,新たに吉城層と考えられる地層の露出を確認した.露頭から採取した凝灰質な砂岩泥岩互層の泥岩部および露頭付近の転石として得られた珪長質な凝灰質泥岩から前期デボン紀Emsianを示す放散虫化石が得られた.従来報告されている吉城層の放散虫化石群集(Zadrappolus yoshikiensis群集)と今回発見された群集から,吉城層の時代は後期シルル紀Pridoliから前期デボン紀Emsianの前期である可能性が高い.この時代論は古城層と福地層がほぼ同時代の地層であることを示す.したがって,両側の接触関係が不整合である可能性は極めて低い.
書誌情報 地質学雑誌
en : 地質学雑誌

巻 109, 号 11, p. 635-647, 発行日 2003-11
出版者
出版者 日本地質学会
ISSN
収録物識別子タイプ ISSN
収録物識別子 00167630
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00141768
権利
権利情報 本文データは学協会の許諾に基づきCiNiiから複製したものである
著者版フラグ
値 publisher
異版である
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://ci.nii.ac.jp/naid/110003009767
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 20:14:26.030022
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