WEKO3
AND
アイテム
{"_buckets": {"deposit": "c2d3c1a7-d124-43c2-a321-c458ce387ca0"}, "_deposit": {"id": "1429", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "1429"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00001429"}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1998-12", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "27", "bibliographicPageStart": "17", "bibliographicVolumeNumber": "45", "bibliographic_titles": [{"bibliographic_title": "The Journal of earth and planetary sciences, Nagoya University"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "CHIME ages were determined for zircon and allanite from the Agigawa welded tuff sheet of the Nohi Rhyolite in the Kamado area, Gifu Prefecture. The CHIME zircon age is 85\u00b15 Ma and the CHIME allanite age is 86\u00b17 Ma. The Agigawa welded tuff sheet in the lowest volcanic sequence of the Nohi Rhyolite is chronologically identical with the post-tectonic Shinshiro Tonalite (85.2\u00b13.3-86.0\u00b14.7 Ma) and the Mitsuhashi Granodiorite (83.8\u00b11.3-84.1\u00b13.1 Ma) in the Ryoke metamorphic belt to the south of the Kamado area. Acidic plutonism and volcanism started simultaneously and widely at about 85 Ma after the high T/P Ryoke metamorphism at about 100 Ma.", "subitem_description_type": "Abstract"}]}, "item_9_description_5": {"attribute_name": "\u5185\u5bb9\u8a18\u8ff0", "attribute_value_mlt": [{"subitem_description": "\u56fd\u7acb\u60c5\u5831\u5b66\u7814\u7a76\u6240\u3067\u96fb\u5b50\u5316\u3057\u305f\u30b3\u30f3\u30c6\u30f3\u30c4\u3092\u4f7f\u7528\u3057\u3066\u3044\u308b\u3002", "subitem_description_type": "Other"}]}, "item_9_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/2840"}]}, "item_9_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.18999/joueps.45.17", "subitem_identifier_reg_type": "JaLC"}]}, "item_9_publisher_32": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "Dept. of Earth and Planetary Sciences, Nagoya University"}]}, "item_9_select_15": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_9_source_id_7": {"attribute_name": "ISSN\uff08print\uff09", "attribute_value_mlt": [{"subitem_source_identifier": "0919875X", "subitem_source_identifier_type": "ISSN"}]}, "item_9_text_14": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Suzuki, Kazuhiro"}], "nameIdentifiers": [{"nameIdentifier": "3333", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Nakazaki, Mineko"}], "nameIdentifiers": [{"nameIdentifier": "3334", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Adachi, Mamoru"}], "nameIdentifiers": [{"nameIdentifier": "3335", "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": "2018-02-16"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000037592.pdf", "filesize": [{"value": "1.6 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 1600000.0, "url": {"label": "KJ00000037592.pdf", "url": "https://nagoya.repo.nii.ac.jp/record/1429/files/KJ00000037592.pdf"}, "version_id": "9045d2b3-ce70-48f1-8df2-97849e5a6321"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "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": "An 85 \u00b1 5 Ma CHIME age for the Agigawa welded tuff sheet in the oldest volcanic sequence of the Nohi Rhyolite, central Japan", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "An 85 \u00b1 5 Ma CHIME age for the Agigawa welded tuff sheet in the oldest volcanic sequence of the Nohi Rhyolite, central Japan"}]}, "item_type_id": "9", "owner": "1", "path": ["336/337/338/345"], "permalink_uri": "https://doi.org/10.18999/joueps.45.17", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_value": "2006-01-05"}, "publish_date": "2006-01-05", "publish_status": "0", "recid": "1429", "relation": {}, "relation_version_is_last": true, "title": ["An 85 \u00b1 5 Ma CHIME age for the Agigawa welded tuff sheet in the oldest volcanic sequence of the Nohi Rhyolite, central Japan"], "weko_shared_id": null}
An 85 ± 5 Ma CHIME age for the Agigawa welded tuff sheet in the oldest volcanic sequence of the Nohi Rhyolite, central Japan
https://doi.org/10.18999/joueps.45.17
c218c5e8-4f07-4a14-8198-ec1fac57fd89
名前 / ファイル | ライセンス | アクション | |
---|---|---|---|
![]() |
|
Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2006-01-05 | |||||
タイトル | ||||||
タイトル | An 85 ± 5 Ma CHIME age for the Agigawa welded tuff sheet in the oldest volcanic sequence of the Nohi Rhyolite, central Japan | |||||
著者 |
Suzuki, Kazuhiro
× Suzuki, Kazuhiro× Nakazaki, Mineko× Adachi, Mamoru |
|||||
抄録 | ||||||
内容記述 | CHIME ages were determined for zircon and allanite from the Agigawa welded tuff sheet of the Nohi Rhyolite in the Kamado area, Gifu Prefecture. The CHIME zircon age is 85±5 Ma and the CHIME allanite age is 86±7 Ma. The Agigawa welded tuff sheet in the lowest volcanic sequence of the Nohi Rhyolite is chronologically identical with the post-tectonic Shinshiro Tonalite (85.2±3.3-86.0±4.7 Ma) and the Mitsuhashi Granodiorite (83.8±1.3-84.1±3.1 Ma) in the Ryoke metamorphic belt to the south of the Kamado area. Acidic plutonism and volcanism started simultaneously and widely at about 85 Ma after the high T/P Ryoke metamorphism at about 100 Ma. | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | 国立情報学研究所で電子化したコンテンツを使用している。 | |||||
内容記述タイプ | Other | |||||
出版者 | ||||||
出版者 | Dept. of Earth and Planetary Sciences, Nagoya University | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.18999/joueps.45.17 | |||||
ID登録タイプ | JaLC | |||||
ISSN(print) | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0919875X | |||||
書誌情報 |
The Journal of earth and planetary sciences, Nagoya University 巻 45, p. 17-27, 発行日 1998-12 |
|||||
フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/2840 | |||||
識別子タイプ | HDL |