WEKO3
アイテム
{"_buckets": {"deposit": "c3678bdc-cc70-4867-90c0-4747dbfa811c"}, "_deposit": {"id": "32676", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32676"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032676", "sets": ["4671", "4672"]}, "author_link": ["126738", "126739", "126736", "126737"], "item_4_alternative_title_1": {"attribute_name": "その他のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "Thermal Structures of the Shikoku Basin and Southwest Japan Subduction Zone"}]}, "item_4_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1999-02-26", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "123", "bibliographicPageStart": "105", "bibliographicVolumeNumber": "73", "bibliographic_titles": [{"bibliographic_title": "東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "フォーマット", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The existing heat flow data in the Shikoku Basin are highly scattered and the average is lower than the value expected from the heat flow versus age relation for normal ocean basins, probably because hydrothermal circulations in the upper crustal layer are not well sealed by sediments. In the Nankai Trough, where the Shikoku Basin lithosphere subducts beneath the southwest Japan arc, the heat flow is too high for its age in the western part, possibly due to heat transfer by fluid flow associated with accretion process, while it appears to be normal in the eastern part. We carried out heat flow measurements in two areas with thick sediment covers at the northeastern end of the Shikoku Basin. The values obtained are quite uniform and agree with the standard heat flow-age relation after correcting for the sedimentation effect. As the crustal structures of the two areas may not be typical of the basin, similar heat flow surveys in the central part of the basin are necessary to know if the thermal structure of the Shikoku Basin lithosphere is normal.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "著者別名", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "126738", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Yamano, Makoto"}]}, {"nameIdentifiers": [{"nameIdentifier": "126739", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Kinoshita, Masataka"}]}]}, "item_4_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15083/0000032676", "subitem_identifier_reg_type": "JaLC"}]}, "item_4_publisher_20": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "東京大学地震研究所"}]}, "item_4_source_id_10": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00162258", "subitem_source_identifier_type": "NCID"}]}, "item_4_source_id_8": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "00408972", "subitem_source_identifier_type": "ISSN"}]}, "item_4_subject_15": {"attribute_name": "日本十進分類法", "attribute_value_mlt": [{"subitem_subject": "453", "subitem_subject_scheme": "NDC"}]}, "item_4_text_21": {"attribute_name": "出版者別名", "attribute_value_mlt": [{"subitem_text_value": "Earthquake Research Institute, University of Tokyo"}]}, "item_4_text_34": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"subitem_text_value": "Departmental Bulletin Paper"}]}, "item_4_text_4": {"attribute_name": "著者所属", "attribute_value_mlt": [{"subitem_text_value": "東京大学地震研究所"}, {"subitem_text_value": "東海大学海洋学部"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "山野, 誠"}], "nameIdentifiers": [{"nameIdentifier": "126736", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "木下, 正高"}], "nameIdentifiers": [{"nameIdentifier": "126737", "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": "2017-06-26"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "ji0731003.pdf", "filesize": [{"value": "2.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 2100000.0, "url": {"label": "ji0731003.pdf", "url": "https://repository.dl.itc.u-tokyo.ac.jp/record/32676/files/ji0731003.pdf"}, "version_id": "718cb3c1-d9f6-4131-bf49-a82397838dfb"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "Shikoku Basin", "subitem_subject_scheme": "Other"}, {"subitem_subject": "southwest Japan", "subitem_subject_scheme": "Other"}, {"subitem_subject": "subduction zone", "subitem_subject_scheme": "Other"}, {"subitem_subject": "thermal structure", "subitem_subject_scheme": "Other"}, {"subitem_subject": "heat flow", "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": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "四国海盆と西南日本沈み込み帯の温度構造について", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "四国海盆と西南日本沈み込み帯の温度構造について", "subitem_title_language": "ja"}]}, "item_type_id": "4", "owner": "1", "path": ["4671", "4672"], "permalink_uri": "https://doi.org/10.15083/0000032676", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2008-05-30"}, "publish_date": "2008-05-30", "publish_status": "0", "recid": "32676", "relation": {}, "relation_version_is_last": true, "title": ["四国海盆と西南日本沈み込み帯の温度構造について"], "weko_shared_id": -1}
四国海盆と西南日本沈み込み帯の温度構造について
https://doi.org/10.15083/0000032676
https://doi.org/10.15083/0000032676f59af40c-65f8-470a-b711-698f9c657eb3
名前 / ファイル | ライセンス | アクション |
---|---|---|
ji0731003.pdf (2.1 MB)
|
|
Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2008-05-30 | |||||
タイトル | ||||||
タイトル | 四国海盆と西南日本沈み込み帯の温度構造について | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | Shikoku Basin | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | southwest Japan | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | subduction zone | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | thermal structure | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | heat flow | |||||
主題Scheme | Other | |||||
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 | 10.15083/0000032676 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Thermal Structures of the Shikoku Basin and Southwest Japan Subduction Zone | |||||
著者 |
山野, 誠
× 山野, 誠× 木下, 正高 |
|||||
著者別名 | ||||||
識別子 | 126738 | |||||
識別子Scheme | WEKO | |||||
姓名 | Yamano, Makoto | |||||
著者別名 | ||||||
識別子 | 126739 | |||||
識別子Scheme | WEKO | |||||
姓名 | Kinoshita, Masataka | |||||
著者所属 | ||||||
著者所属 | 東京大学地震研究所 | |||||
著者所属 | ||||||
著者所属 | 東海大学海洋学部 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The existing heat flow data in the Shikoku Basin are highly scattered and the average is lower than the value expected from the heat flow versus age relation for normal ocean basins, probably because hydrothermal circulations in the upper crustal layer are not well sealed by sediments. In the Nankai Trough, where the Shikoku Basin lithosphere subducts beneath the southwest Japan arc, the heat flow is too high for its age in the western part, possibly due to heat transfer by fluid flow associated with accretion process, while it appears to be normal in the eastern part. We carried out heat flow measurements in two areas with thick sediment covers at the northeastern end of the Shikoku Basin. The values obtained are quite uniform and agree with the standard heat flow-age relation after correcting for the sedimentation effect. As the crustal structures of the two areas may not be typical of the basin, similar heat flow surveys in the central part of the basin are necessary to know if the thermal structure of the Shikoku Basin lithosphere is normal. | |||||
書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 73, 号 1, p. 105-123, 発行日 1999-02-26 |
|||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00162258 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
日本十進分類法 | ||||||
主題 | 453 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, University of Tokyo |