{"created":"2023-07-27T06:26:31.969287+00:00","id":10287,"links":{},"metadata":{"_buckets":{"deposit":"a68dfc27-4879-4db0-9ff9-83e5ff0b3319"},"_deposit":{"created_by":3,"id":"10287","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"10287"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00010287","sets":["934:935:937"]},"author_link":["15425","15427","15426"],"item_4_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2007-04-16","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"7","bibliographicPageEnd":"24","bibliographicPageStart":"1","bibliographicVolumeNumber":"34","bibliographic_titles":[{"bibliographic_title":"Geophysical Research Letters"}]}]},"item_4_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"We investigate a duration-amplitude relation of non-volcanic deep low-frequency (DLF) tremors in the Tokai region, southwest Japan, to constrain the source process of the tremors. We apply two models to the distribution, one is an exponential model as a scale bound distribution and the other a power law model as a scale invariant distribution. The exponential model shows a better fit to the duration-amplitude distribution of the tremors than a power law model, implying that the DLF tremors are caused by a scale-bound source process. The source process of the DLF tremors, therefore, differs from those for earthquakes. We suggest that the non-volcanic DLF tremor is possibly caused by a fixed source dimension with variable excess pressure of fluid or variable stress drop. Copyright 2007 by the American Geophysical Union.","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学大学院自然科学研究科自然計測","subitem_description_type":"Other"},{"subitem_description":"金沢大学理学部","subitem_description_type":"Other"}]},"item_4_publisher_17":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"American Geophysical Union"}]},"item_4_relation_12":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type":"isVersionOf","subitem_relation_type_id":{"subitem_relation_type_id_text":"10.1029/2007GL029391","subitem_relation_type_select":"DOI"}}]},"item_4_relation_27":{"attribute_name":"シリーズ","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"L07305"}]}]},"item_4_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0094-8276","subitem_source_identifier_type":"ISSN"}]},"item_4_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_ab4af688f83e57aa","subitem_version_type":"AM"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Watanabe, Tomoko"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Hiramatsu, Yoshizo"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Obara, Kazushige"}],"nameIdentifiers":[{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-10-03"}],"displaytype":"detail","filename":"SC-PR-HIRAMATSU-Y-37.pdf","filesize":[{"value":"677.3 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"SC-PR-HIRAMATSU-Y-37.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/10287/files/SC-PR-HIRAMATSU-Y-37.pdf"},"version_id":"1c557e68-9db1-4f55-8008-de36d576e1f7"}]},"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":"Scaling relationship between the duration and the amplitude of non-volcanic deep low-frequency tremors","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Scaling relationship between the duration and the amplitude of non-volcanic deep low-frequency tremors"}]},"item_type_id":"4","owner":"3","path":["937"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-10-03"},"publish_date":"2017-10-03","publish_status":"0","recid":"10287","relation_version_is_last":true,"title":["Scaling relationship between the duration and the amplitude of non-volcanic deep low-frequency tremors"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-07-28T01:42:19.354398+00:00"}