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": "6eca9617-5ae5-4d1d-bacf-5674da82a351"}, "_deposit": {"id": "11871", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "11871"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00011871", "sets": ["1170"]}, "author_link": ["36356", "36357", "36358"], "control_number": "11871", "item_1628147817048": {"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_6_alternative_title_1": {"attribute_name": "その他(別言語等)のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "西南日本, 紀伊半島四万十帯北縁より白亜紀浅海性二枚貝の産出"}]}, "item_6_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1979-04-30", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "29", "bibliographicPageStart": "15", "bibliographicVolumeNumber": "113", "bibliographic_titles": [{"bibliographic_title": "日本古生物学会報告・紀事 新篇"}]}]}, "item_6_description_20": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "和歌山県清水町の湯川川下流, 湯川層砂岩よりSpondylus aff. decoratus, Plicatula aff. hanaii, Amphidonte cf. subhaliotoidea, Ostrea sp.などの二枚貝や, さんごCamalophyllia sp.が発見された。二枚貝は宮古統のものに類似し, 時代は古白亜紀とみなされる。厚殻, 付着, 固着性の二枚貝を主体とし, ごく浅い海の環境を示している。これは砂岩の堆積学的研究からも支持される。周囲はやや深い地向斜性の堆積層であるが, このような浅海性の地層の存在は, 海底地辷りによるものではなく, 海水準の相対的変化によるものと結論した。  Bivalve fossils collected from the northern border of the Shimanto Terrain are characterised by shallow marine species, such as Spondylus aff. decoratus, Plicatula aff. hanaii, Amphidonte cf. subhaliotoidea, Rastellum? sp., Ostrea sp. and others, the age of which is considered to be early Cretaceous. The fossilbearing sandstones also show a shallow shelf environment, while the surrounding sandstones indicate turbidity current origin under bathyal environment. The presence of shallow-sea sediments among the turbidite sequence is explained by sealevel change and not by submarine slide of the shallow-sea sediments.", "subitem_description_type": "Abstract"}]}, "item_6_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_6_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_6_description_5": {"attribute_name": "引用", "attribute_value_mlt": [{"subitem_description": "日本古生物学会報告・紀事 新篇. 113:15-29 (1979)", "subitem_description_type": "Other"}]}, "item_6_link_3": {"attribute_name": "信州大学研究者総覧へのリンク", "attribute_value_mlt": [{"subitem_link_text": "Kumon, Fujio", "subitem_link_url": "http://soar-rd.shinshu-u.ac.jp/profile/ja.ZUchOUkh.html"}]}, "item_6_publisher_4": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "日本古生物学会"}]}, "item_6_relation_48": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type": "isIdenticalTo", "subitem_relation_type_id": {"subitem_relation_type_id_text": "https://doi.org/10.14825/prpsj1951.1979.113_15", "subitem_relation_type_select": "DOI"}}]}, "item_6_relation_51": {"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/110002703091/", "subitem_relation_type_select": "URI"}}]}, "item_6_rights_62": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "日本古生物学会"}, {"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_6_select_64": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_6_source_id_35": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0031-0204", "subitem_source_identifier_type": "PISSN"}]}, "item_6_source_id_39": {"attribute_name": "NII ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0031-0204", "subitem_source_identifier_type": "PISSN"}]}, "item_6_source_id_40": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AA00867896", "subitem_source_identifier_type": "NCID"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Nakazawa,  Kenji"}], "nameIdentifiers": [{"nameIdentifier": "36356", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kumon,  Fujio"}], "nameIdentifiers": [{"nameIdentifier": "36357", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kimura,  Katsumi"}], "nameIdentifiers": [{"nameIdentifier": "36358", "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": "OCCURRENCE_CRETACEOUS_SHALLOW-SEA_BIVALVES.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": "OCCURRENCE_CRETACEOUS_SHALLOW-SEA_BIVALVES.pdf", "url": "https://soar-ir.repo.nii.ac.jp/record/11871/files/OCCURRENCE_CRETACEOUS_SHALLOW-SEA_BIVALVES.pdf"}, "version_id": "27b84ebb-8e4a-4e4c-903c-4fed5f9508ae"}]}, "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": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "OCCURRENCE OF CRETACEOUS SHALLOW-SEA BIVALVES FROM THE NORTHERN BORDER OF SHIMANTO TERRAIN, KII PENINSULA, SOUTHWEST JAPAN", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "OCCURRENCE OF CRETACEOUS SHALLOW-SEA BIVALVES FROM THE NORTHERN BORDER OF SHIMANTO TERRAIN, KII PENINSULA, SOUTHWEST JAPAN", "subitem_title_language": "en"}]}, "item_type_id": "6", "owner": "1", "path": ["1170"], "permalink_uri": "http://hdl.handle.net/10091/12017", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2011-03-10"}, "publish_date": "2011-03-10", "publish_status": "0", "recid": "11871", "relation": {}, "relation_version_is_last": true, "title": ["OCCURRENCE OF CRETACEOUS SHALLOW-SEA BIVALVES FROM THE NORTHERN BORDER OF SHIMANTO TERRAIN, KII PENINSULA, SOUTHWEST JAPAN"], "weko_shared_id": -1}
  1. 040 理学部
  2. 0401 学術論文

OCCURRENCE OF CRETACEOUS SHALLOW-SEA BIVALVES FROM THE NORTHERN BORDER OF SHIMANTO TERRAIN, KII PENINSULA, SOUTHWEST JAPAN

http://hdl.handle.net/10091/12017
http://hdl.handle.net/10091/12017
da155880-4da7-4f44-b991-68418a558679
名前 / ファイル ライセンス アクション
OCCURRENCE_CRETACEOUS_SHALLOW-SEA_BIVALVES.pdf OCCURRENCE_CRETACEOUS_SHALLOW-SEA_BIVALVES.pdf (2.2 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2011-03-10
タイトル
言語 en
タイトル OCCURRENCE OF CRETACEOUS SHALLOW-SEA BIVALVES FROM THE NORTHERN BORDER OF SHIMANTO TERRAIN, KII PENINSULA, SOUTHWEST JAPAN
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
その他(別言語等)のタイトル
その他のタイトル 西南日本, 紀伊半島四万十帯北縁より白亜紀浅海性二枚貝の産出
著者 Nakazawa, Kenji

× Nakazawa, Kenji

WEKO 36356

Nakazawa, Kenji

Search repository
Kumon, Fujio

× Kumon, Fujio

WEKO 36357

Kumon, Fujio

Search repository
Kimura, Katsumi

× Kimura, Katsumi

WEKO 36358

Kimura, Katsumi

Search repository
信州大学研究者総覧へのリンク
氏名 Kumon, Fujio
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.ZUchOUkh.html
出版者
出版者 日本古生物学会
引用
内容記述タイプ Other
内容記述 日本古生物学会報告・紀事 新篇. 113:15-29 (1979)
書誌情報 日本古生物学会報告・紀事 新篇

巻 113, p. 15-29, 発行日 1979-04-30
抄録
内容記述タイプ Abstract
内容記述 和歌山県清水町の湯川川下流, 湯川層砂岩よりSpondylus aff. decoratus, Plicatula aff. hanaii, Amphidonte cf. subhaliotoidea, Ostrea sp.などの二枚貝や, さんごCamalophyllia sp.が発見された。二枚貝は宮古統のものに類似し, 時代は古白亜紀とみなされる。厚殻, 付着, 固着性の二枚貝を主体とし, ごく浅い海の環境を示している。これは砂岩の堆積学的研究からも支持される。周囲はやや深い地向斜性の堆積層であるが, このような浅海性の地層の存在は, 海底地辷りによるものではなく, 海水準の相対的変化によるものと結論した。 Bivalve fossils collected from the northern border of the Shimanto Terrain are characterised by shallow marine species, such as Spondylus aff. decoratus, Plicatula aff. hanaii, Amphidonte cf. subhaliotoidea, Rastellum? sp., Ostrea sp. and others, the age of which is considered to be early Cretaceous. The fossilbearing sandstones also show a shallow shelf environment, while the surrounding sandstones indicate turbidity current origin under bathyal environment. The presence of shallow-sea sediments among the turbidite sequence is explained by sealevel change and not by submarine slide of the shallow-sea sediments.
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 0031-0204
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00867896
DOI
関連タイプ isIdenticalTo
識別子タイプ DOI
関連識別子 https://doi.org/10.14825/prpsj1951.1979.113_15
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/110002703091/
権利
権利情報 日本古生物学会
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
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 11:40:14.088544
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