ログイン
言語:

WEKO3

  • トップ
  • コミュニティ
  • ランキング
AND
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": "7181853a-710f-4524-9e92-2fb56f49f845"}, "_deposit": {"id": "32972", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32972"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032972", "sets": []}, "author_link": ["128560", "128559"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "\u7e26\u305a\u308c\u578b\u6df1\u767a\u5730\u9707\u306b\u3088\u3063\u3066\u52b1\u8d77\u3055\u308c\u308b\u5408\u6210\u6d77\u6d0b\u6027\u30ec\u30a4\u30ea\u30fc\u6ce2\u306e\u4e00\u6b21\u9ad8\u6b21\u30e2\u30fc\u30c9\u306e\u30b9\u30da\u30af\u30c8\u30eb"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1983-03-31", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "625", "bibliographicPageStart": "609", "bibliographicVolumeNumber": "57", "bibliographic_titles": [{"bibliographic_title": "\u6771\u4eac\u5927\u5b78\u5730\u9707\u7814\u7a76\u6240\u5f59\u5831 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "For the purpose of understanding the excitation of the first higher mode of oceanic Rayleigh waves, the waves are simulated for the seismic sources with a pure dip-slip motion along a vertical fault plane, for various focal depths from 10 to 500 km. It is suggested that the first higher mode of oceanic Rayleigh waves generated by deep earthquakes with the focal depth of about 200 or 300 km can be observed in the period range from 20 to 50 seconds, with the amplitude exceeding that of the fundamental mode. The optimum filtering parameters for the analysis of dispersed oceannic Rayleigh waves are determined by using the simulated Rayleigh waves of the fundamental and first higher modes. The filtering parameters will be used most effectively for the determination of the group velocity dispersion curves of oceanic surface waves.", "subitem_description_type": "Abstract"}, {"subitem_description": "\u6d77\u6d0b\u6027\u4e00\u6b21\u9ad8\u6b21\u30e2\u30fc\u30c9\u30ec\u30ea\u30fc\u6ce2\u306e\u52b1\u8d77\u306b\u3064\u3044\u3066\u7406\u89e3\u3059\u308b\u70ba\u306b,\u9707\u6e90\u306e\u6df1\u3055\u309210km\u304b\u3089500km\u307e\u3067\u6570\u591a\u304f\u3068\u308a,\u7d14\u7c8b\u306a\u7e26\u305a\u308c\u65ad\u5c64\u578b\u306e\u9707\u6e90\u3092\u4eee\u5b9a\u3057\u3066\u5408\u6210\u6ce2\u3092\u5f97\u305f.\u305d\u308c\u306b\u3088\u308c\u3070,\u9707\u6e90\u306e\u6df1\u3055\u304c\u7d04200km\u304b\u3089300km\u306e\u6df1\u767a\u5730\u9707\u306b\u3088\u3063\u3066\u751f\u6210\u3055\u308c\u308b\u6d77\u6d0b\u6027\u4e00\u6b21\u9ad8\u6b21\u30e2\u30fc\u30c9\u30ec\u30a4\u30ea\u30fc\u6ce2\u306f\u5468\u671f20\u79d2\u304b\u308950\u79d2\u306e\u7bc4\u56f2\u3067\u89b3\u6e2c\u53ef\u80fd\u3067\u3042\u308b\u4e8b\u304c\u671f\u5f85\u3055\u308c,\u305d\u306e\u632f\u5e45\u306f\u57fa\u672c\u30e2\u30fc\u30c9\u3092\u8d8a\u3048\u3066\u3044\u308b.\u5206\u6563\u3057\u305f\u6d77\u6d0b\u6027\u30ec\u30a4\u30ea\u30fc\u6ce2\u3092\u89e3\u6790\u3059\u308b\u70ba\u306e\u6700\u9069\u30d5\u30a3\u30eb\u30bf\u30ea\u30f3\u30b0\u30d1\u30e9\u30e1\u30fc\u30bf\u304c,\u5408\u6210\u3055\u308c\u305f\u57fa\u672c\u53ca\u3073\u4e00\u6b21\u9ad8\u6b21\u30e2\u30fc\u30c9\u30ec\u30a4\u30ea\u30fc\u6ce2\u3092\u4f7f\u3063\u3066\u6c7a\u5b9a\u3055\u308c\u305f.\u3053\u306e\u30d5\u30a3\u30eb\u30bf\u30ea\u30f3\u30b0\u30d1\u30e9\u30e1\u30fc\u30bf\u306f\u6d77\u6d0b\u6027\u8868\u9762\u6ce2\u306e\u7fa4\u901f\u5ea6\u5206\u6563\u66f2\u7dda\u6c7a\u5b9a\u306e\u969b\u306b\u6700\u3082\u52b9\u679c\u7684\u306b\u4f7f\u308f\u308c\u308b.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "128560", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "\u5409\u7530, \u6e80"}]}]}, "item_4_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15083/0000032972", "subitem_identifier_reg_type": "JaLC"}]}, "item_4_publisher_20": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "\u6771\u4eac\u5927\u5b66\u5730\u9707\u7814\u7a76\u6240"}]}, "item_4_source_id_10": {"attribute_name": "\u66f8\u8a8c\u30ec\u30b3\u30fc\u30c9ID", "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": "\u65e5\u672c\u5341\u9032\u5206\u985e\u6cd5", "attribute_value_mlt": [{"subitem_subject": "453", "subitem_subject_scheme": "NDC"}]}, "item_4_text_21": {"attribute_name": "\u51fa\u7248\u8005\u5225\u540d", "attribute_value_mlt": [{"subitem_text_value": "Earthquake Research Institute, University of Tokyo"}]}, "item_4_text_34": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_text_value": "Departmental Bulletin Paper"}]}, "item_4_text_4": {"attribute_name": "\u8457\u8005\u6240\u5c5e", "attribute_value_mlt": [{"subitem_text_value": "\u5730\u9707\u7814\u7a76\u6240"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Yoshida, Mitsuru"}], "nameIdentifiers": [{"nameIdentifier": "128559", "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": "2017-06-26"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "ji0574001.pdf", "filesize": [{"value": "956.3 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 956300.0, "url": {"label": "ji0574001.pdf", "url": "https://repository.dl.itc.u-tokyo.ac.jp/record/32972/files/ji0574001.pdf"}, "version_id": "9d43de22-422b-4806-bcdd-99fd5c266b6f"}]}, "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": "Spectra of the First Higher Mode of Simulated Oceanic Rayleigh Waves Generated by Deep Earthquakes of the Dip-Slip Type", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "Spectra of the First Higher Mode of Simulated Oceanic Rayleigh Waves Generated by Deep Earthquakes of the Dip-Slip Type", "subitem_title_language": "en"}]}, "item_type_id": "4", "owner": "1", "path": ["80/4535/4807/4808", "9/504/4538/4809/4810"], "permalink_uri": "https://doi.org/10.15083/0000032972", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2008-05-30"}, "publish_date": "2008-05-30", "publish_status": "0", "recid": "32972", "relation": {}, "relation_version_is_last": true, "title": ["Spectra of the First Higher Mode of Simulated Oceanic Rayleigh Waves Generated by Deep Earthquakes of the Dip-Slip Type"], "weko_shared_id": -1}
  1. 131 地震研究所
  2. 東京大学地震研究所彙報
  3. 57
  4. 4
  1. 0 資料タイプ別
  2. 30 紀要・部局刊行物
  3. 東京大学地震研究所彙報
  4. 57
  5. 4

Spectra of the First Higher Mode of Simulated Oceanic Rayleigh Waves Generated by Deep Earthquakes of the Dip-Slip Type

https://doi.org/10.15083/0000032972
3e62021f-4509-4a70-8463-21a7a92da62b
名前 / ファイル ライセンス アクション
ji0574001.pdf ji0574001.pdf (956.3 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-05-30
タイトル
タイトル Spectra of the First Higher Mode of Simulated Oceanic Rayleigh Waves Generated by Deep Earthquakes of the Dip-Slip Type
言語 en
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 10.15083/0000032972
ID登録タイプ JaLC
その他のタイトル
その他のタイトル 縦ずれ型深発地震によって励起される合成海洋性レイリー波の一次高次モードのスペクトル
著者 Yoshida, Mitsuru

× Yoshida, Mitsuru

WEKO 128559

Yoshida, Mitsuru

Search repository
著者別名
識別子
識別子 128560
識別子Scheme WEKO
姓名
姓名 吉田, 満
著者所属
著者所属 地震研究所
抄録
内容記述タイプ Abstract
内容記述 For the purpose of understanding the excitation of the first higher mode of oceanic Rayleigh waves, the waves are simulated for the seismic sources with a pure dip-slip motion along a vertical fault plane, for various focal depths from 10 to 500 km. It is suggested that the first higher mode of oceanic Rayleigh waves generated by deep earthquakes with the focal depth of about 200 or 300 km can be observed in the period range from 20 to 50 seconds, with the amplitude exceeding that of the fundamental mode. The optimum filtering parameters for the analysis of dispersed oceannic Rayleigh waves are determined by using the simulated Rayleigh waves of the fundamental and first higher modes. The filtering parameters will be used most effectively for the determination of the group velocity dispersion curves of oceanic surface waves.
抄録
内容記述タイプ Abstract
内容記述 海洋性一次高次モードレリー波の励起について理解する為に,震源の深さを10kmから500kmまで数多くとり,純粋な縦ずれ断層型の震源を仮定して合成波を得た.それによれば,震源の深さが約200kmから300kmの深発地震によって生成される海洋性一次高次モードレイリー波は周期20秒から50秒の範囲で観測可能である事が期待され,その振幅は基本モードを越えている.分散した海洋性レイリー波を解析する為の最適フィルタリングパラメータが,合成された基本及び一次高次モードレイリー波を使って決定された.このフィルタリングパラメータは海洋性表面波の群速度分散曲線決定の際に最も効果的に使われる.
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 57, 号 4, p. 609-625, 発行日 1983-03-31
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
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 22:00:10.596418
Show All versions

Share

Mendeley CiteULike Twitter Facebook Print Addthis

Cite as

Export

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

Confirm


Powered by CERN Data Centre & Invenio


Powered by CERN Data Centre & Invenio